RNS Number : 2178R
Castillo Copper Limited
28 February 2023
 

A picture containing text, clipart Description automatically generated


28 February 2023

 

 

 

CASTILLO COPPER LIMITED
("Castillo", or the "Company")

 

Encouraging REE metallurgy test-work from Broken Hill  

 

Castillo Copper Limited (LSE and ASX: CCZ), a base metal explorer primarily focused on copper across Australia and Zambia, is pleased to announce encouraging results from initial Rare Earth Element ("REE") metallurgical test-work at the Fence Gossan Prospect (Appendix A) within the BHA Project's East Zone.

 

HIGHLIGHTS:

·    Preliminary metallurgical test-work on a 20m composite sample from the Fence Gossan Prospect (FG_003RC) delivered encouraging results, with clays - subjected to froth flotation - obtaining up to 2-3 times REE enrichment from the head grade at up to 70% recovery (refer Figure 1 and Appendix B for full details):

These findings confirm REEs can be readily separated from clay within the East Zone discovery area and potentially beneficiated to a higher grade concentrate

 

·    To acquire a deeper understanding of the potential to extract REE-mineralisation from clays in the East Zone discovery area, the Board has approved appointing a specialist consultancy to conduct an in-depth metallurgy test-work programme:

Once completed and interpreted, the results from this programme will be key to securing interest from potential off-take partners and providing a path to market

 

·    Further, 1m re-assays for Reefs Tank were received for all four drill-holes (RT_001-4RC), which further verified there is an extensive, shallow REE system apparent across the central part of the East Zone - the best intercept comprised:

3m @ 2,587ppm TREO from 14m (RT_001RC)

 

·    Reconciling all assays from the recent drilling and auger campaigns across the Fence Gossan, Tors and Reefs Tanks Prospects, the geology team has created heat maps which identify zones of high Total and Magnetic Rare Earth Oxides ("TREO"/"MREO"):

o These areas will be subject to further surface sampling and geophysical surveys then potentially drill-testing to extend known mineralisation

 

Ged Hall, Chairman of Castillo Copper, said: "On a holistic basis, the Board is delighted with results from the drilling, surface sampling and metallurgical test-work at Broken Hill as they collectively demonstrate the forward value creating potential of the BHA Project's East Zone. In short, the underlying REE system is shallow, extends over at least 4.5km2, delivered results up to 3,491ppm TREO and produced up to 38.9% MREO in diamond core1. Moreover, the metallurgy test-work proves REE mineralisation readily separates from clay and can potentially be beneficiated to a higher-grade concentrate. By all accounts, this is an excellent report card ahead of exploratory work ramping up."

 

ENCOURAGING METALLURGICAL TEST-WORK RESULTS

FIGURE A1: HEAD ASSAY / IMPROVEMENT

ANALYTE

ALS Adelaide

REE ME-MS81

%

ALS Perth

HEAD GRADE REE COMP %

Times Improvement

Ce (%)

0.045

0.05

1.6

La (%)

0.038

0.03

2.3

Nd (%)

0.021

0.02

2.0

Pr (%)

0.006

0.01

1.3

Y (%)

0.009

0.01

1.1

 

 

 

 

 

 

Source: ALS

To follow up on these excellent results, the Board has now approved the appointment of a specialist metallurgy consultancy with extensive experience in how REE mineralisation liberates from various host rocks (including clays). The Board wants a deeper understanding of the potential to extract REE mineralisation from the East Zone discovery area, as this information will be key to securing interest from potential off-take partners that can provide a clear path to market.   

Reefs Tank Assays

All 1m re-assays for Reefs Tank were received for the four drill-holes (RT_001-4RC), with up to 2,587ppm TREO recorded (Figure 1). On a holistic basis, the Reefs Tank results provide incremental evidence there is an extensive, shallow REE system apparent across the central part of the BHA Project's East Zone (Appendix A).

FIGURE 1:  REEFS TANK 1M ASSAYS

Hole

From (m)

To (m)

Width (m)

Ag

(g/t)

Th (ppm)

U (ppm)

TREO (ppm)

TREO-Ce (ppm)

LREO (ppm)

HREO (ppm)

CREO

(%)

MREO

(%)

RT_001RC

11

13

2

0.05

17.0

5.4

631

313.08

490.55

140.69

27.3%

20.6%

RT_001RC

14

17

3

0.96

29.9

9.4

2,587

2187.30

1105.24

1481.70

55.7%

24.7%

RT_001RC

54

55

1

0.15

70.2

9.2

796

429.43

746.15

49.34

20.8%

29.1%

RT_001RC

55

56

1

0.08

80.5

6.2

896

487.84

838.19

57.49

21.2%

29.9%

RT_001RC

64

65

1

0.12

121.0

9.0

1,236

658.75

1196.01

40.09

19.0%

29.3%

RT_002RC

0

1

1

0.06

19.8

2.5

367

241.55

272.76

94.70

34.1%

28.2%

RT_002RC

1

4

3

0.11

24.7

2.5

449

285.00

350.63

98.36

31.5%

27.6%

RT_002RC

28

32

4

0.12

54.6

3.5

601

343.27

541.76

59.48

24.1%

30.9%

RT_002RC

64

68

4

0.05

27.6

3.2

430

267.15

339.41

90.36

30.7%

27.5%

RT_003RC

0

4

4

nd

14.6

6.2

247

165.15

183.62

63.40

34.5%

29.8%

RT_003RC

8

16

8

nd

27.5

4.5

424

258.35

352.12

71.76

28.4%

28.5%

RT_003RC

56

64

8

nd

23.8

3.8

389

237.70

313.43

75.97

29.6%

27.6%

RT_003RC

72

76

4

nd

28.6

6.9

450

272.82

366.14

83.72

29.1%

27.3%

RT_004RC

52

56

4

0.25

44.4

4.1

567

344.40

465.92

101.13

29.1%

29.2%

RT_004RC

84

92

8

1.78

25.6

8.5

525

314.92

433.13

92.23

28.4%

27.7%

 Source: CCZ geology team

 

 

TREO / MREO Contours

After reconciling all assays from the recent drilling and auger campaigns across the Fence Gossan, Tors & Reefs Tanks Prospects (Appendix B), the geology team has created heat maps which identify zones of high TREO and MREO (Figure 2 & 3).

These areas will be subject to further surface sampling and geophysical campaigns (including trial transects of ground radiometric and EM surveys) then potentially drill-testing (red zones in Figure 2) to extend known mineralisation.

Note, the TREO is the sum of REEs in ppm, calculated from ME-MS81 method, converted to their stoichiometric equivalent i.e., Ce converted to CeO2 and so forth. The high-value Magnetic REO comprise Nd+Pr+Dy+Tb and generally command premium pricing to other REEs as they are in strong demand. Refer to Appendix C for a full explanation and TREO calculation.

FIGURE 2: FENCE GOSSAN AND SURROUNDS SURFACE SAMPLING - TREO IN PPM

A picture containing chart Description automatically generated

Source: CCZ geology team

 

 

 

 

 

 

FIGURE 3: FENCE GOSSAN AND SURROUNDS SURFACE SAMPLING - MREO ppm

Map Description automatically generated

Notes: All coordinates in MGA94-Z54S Source: CCZ Geology team



 

For further information, please contact:  

 

Castillo Copper Limited  

+61 8 6558 0886  

Dr Dennis Jensen (Australia), Managing Director  

Gerrard Hall (UK), Chairman  

  

  

  

SI Capital Limited (Financial Adviser and Corporate Broker)  

+44 (0)1483 413500  

Nick Emerson  

  


  

Gracechurch Group (Financial PR) 

+44 (0)20 4582 3500

Harry Chathli, Alexis Gore, Henry Gamble 

 

  

 

About Castillo Copper  

 

Castillo Copper Limited is an Australian-based explorer primarily focused on copper across Australia and Zambia. The group is embarking on a strategic transformation to morph into a mid-tier copper group underpinned by its core projects:  

  

·    A large footprint in the Mt Isa copper-belt district, north-west Queensland, which delivers significant exploration upside through having several high-grade targets and a sizeable untested anomaly within its boundaries in a copper-rich region.  

·    Four high-quality prospective assets across Zambia's copper-belt which is the second largest copper producer in Africa.  

·    A large tenure footprint proximal to Broken Hill's world-class deposit that is prospective for zinc-silver-lead-copper-gold and platinoids.   

·    Cangai Copper Mine in northern New South Wales, which is one of Australia's highest grading historic copper mines.  

 

The group is listed on the LSE and ASX under the ticker "CCZ."  

 

Competent Person's Statement

The information in this report that relates to Exploration Results and Mineral Resource Estimates for "BHA Project, East Zone" is based on information compiled or reviewed by Mr Mark Biggs.  Mr Biggs is a director of ROM Resources, a company which is a shareholder of Castillo Copper Limited.  ROM Resources provides ad hoc geological consultancy services to Castillo Copper Limited.  Mr Biggs is a member of the Australian Institute of Mining and Metallurgy (member #107188) and has sufficient experience of relevance to the styles of mineralisation and types of deposits under consideration, and to the activities undertaken, to qualify as a Competent Person as defined in the 2012 Edition of the Joint Ore Reserves Committee (JORC) Australasian Code for Reporting of Exploration Results, and Mineral Resources. Mr Biggs holds an AusIMM Online Course Certificate in 2012 JORC Code Reporting.  Mr Biggs also consents to the inclusion in this report of the matters based on information in the form and context in which it appears.

References

1)        CCZ ASX Release - 15 February 2023

 

 

 

 

 

APPENDIX A: BHA PROJECT'S EAST ZONE

FIGURE A1: BHA PROJECT's EAST ZONE - REE EXPLORATION FOOTPRINT

Diagram, schematic Description automatically generated

Source: CCZ geology team

FIGURE A2: BHA PROJECT

Diagram Description automatically generated

Source: CCZ geology team

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

APPENDIX B: PRELIMINARY METALLURGY TESTWORK

Background and Scope

A composite sample of RC chips from Fence Gossan drill-hole FG_003RC was constructed over the interval from 0-20m. The material reported over that interval had lithology logged as clay, haematite, goethite, and extremely weathered pegmatite. The main rare-containing minerals are thought to be monazite, allanite, xenotime, and possibly baryte or celsian (to account for the high barium contents of some samples). Note, these assumptions need to be tested by XRD and/or QEM-SEM testing. 

The composite was made up of 1m samples tested using ME-MS81 analysis method (the results for which are provided in Figure A1).

The process methodology followed by ALS Perth was as follows:

·    Rotary Blending & Splitting (12x1kg, reserve)

·    PPS - Head Assay Submission

·    Assay - Head Assay (Ce, La, Nd, Pr, SiO2, Y)

·    1kg Grind Establishment (P80 53μm assumed)

·    Rougher Flotation (6 con, 1 Tail)

·    PPS - Float Products

·    Assay - Head Assay (Ce, La, Nd, Pr, SiO2, and Y)

Results

The head grade and froth flotation improvement are shown in Figure A1. 

FIGURE A1: HEAD ASSAY / IMPROVEMENT

ANALYTE

ALS Adelaide

REE ME-MS81

%

ALS Perth

HEAD GRADE REE COMP %

Times Improvement

Ce (%)

0.045

0.05

1.6

La (%)

0.038

0.03

2.3

Nd (%)

0.021

0.02

2.0

Pr (%)

0.006

0.01

1.3

SiO2 (%)

NT

64.3

-

Y (%)

0.009

0.01

1.1

 

 

 

 

 

 

 

Source: ALS

Overall main laboratory observations of note are:

·    Slurry was highly viscous after ALS Perth added lime that changed the target pH down to 9.5. The process was changed to soda ash in the second test.

·    By end of float, ALS Perth saw froth instability, which indicates what material wanted to float.

·    There was a colour trend in the concentrate progressing through the stages.

Figures A2 to A5 show cumulative recovery versus grade for the Ce, La, Nd, and Pr components.

 

FIGURE A1: CERIUM CUMULATIVE GRADE / RECOVERY

Source: ALS

FIGURE A1: LANTHANUM CUMULATIVE GRADE / RECOVERY

Source: ALS

 

FIGURE A1: NEODYMIUM UMULATIVE GRADE / RECOVERY

Source: ALS

FIGURE A5: PRASEODYMIUM CUMULATIVE GRADE / RECOVERY

Source: ALS



FIGURE A6: FLOWTATION FLOWSHEET

Graphical user interface, table Description automatically generated with medium confidence

Source: ALS


FIGURE A7: DRILLHOLE FG_003RC - 0 TO 20M COMPOSITE USED FOR ALS PERTH METALLURGICAL TESTING, 1M ANALYSIS (A-P)

Sample

Number

From

To

Length

PGM-MS23

PGM-MS23

PGM-MS23

ME-MS81

ME-MS81

ME-MS81

ME-MS81

ME-MS81

ME-MS81

ME-MS81

ME-MS81

ME-MS81

ME-MS81

ME-MS81

ME-MS81

ME-MS81

ME-MS81

ME-MS81

ME-MS81

 




Au

Pt

Pd

Ba

Ce

Cr

Cs

Dy

Er

Eu

Ga

Gd

Hf

Ho

La

Lu

Nb

Nd

Pr

 

m

m

m

ppm

ppm

ppm

ppm

ppm

ppm

ppm

ppm

ppm

ppm

ppm

ppm

ppm

ppm

ppm

ppm

ppm

ppm

ppm

CCZ04511

0

1

1

0.002

0.001

0.002

297

131

61

3.13

6.48

3.92

1.71

23.5

7.17

5.56

1.35

70

0.58

10.85

54.8

16.1

CCZ04512

1

2

1

0.006

0.0013

0.003

910

172.5

73

2.58

7.57

4.05

2.16

38.1

8.71

4.09

1.52

97.5

0.46

10.55

74.2

21

CCZ04513

2

3

1

0.004

0.0011

0.002

648

696

71

2.64

20.9

9.3

9.12

46.2

34.4

4.18

3.6

409

0.93

12.75

347

94.2

CCZ04514

3

4

1

0.002

0.0007

0.001

166.5

580

72

5.2

17.85

6.75

7.5

55.9

28.5

3.02

2.76

369

0.54

10.4

276

74.4

CCZ04515

4

5

1

0.002

0.0007

0.001

143

511

80

5.01

16.35

6.43

6.46

51.2

25.9

3.39

2.67

336

0.63

13.85

252

67.4

CCZ04516

5

6

1

0.001

0.0008

0.001

98.4

376

75

3.04

10.5

3.86

3.91

53.5

17.5

3.05

1.62

229

0.36

12.8

175.5

46.6

CCZ04517

6

7

1

<0.001

0.0008

0.001

91.9

480

76

3.89

13.75

4.51

5.55

54.5

22.4

3.37

2.03

293

0.47

11.9

221

59.8

CCZ04518

7

8

1

<0.001

0.0007

0.001

59.1

332

90

3.2

8.64

3.14

3.43

60.5

14.3

3.18

1.33

204

0.28

15.4

142.5

39.3

CCZ04519

8

9

1

<0.001

0.0007

0.001

87.2

422

88

5.13

12.5

5.17

4.67

53.4

19

2.97

2.05

258

0.6

12.55

184.5

49.7

CCZ04520

9

10

1

<0.001

0.0008

0.001

94.5

287

78

5.62

7.68

3.76

2.49

56.5

10.55

2.62

1.37

175

0.49

13.2

116.5

31.3

CCZ04521

10

11

1

0.001

0.0007

0.001

110.5

366

81

6.57

8.9

4.09

3.31

48.3

14.05

2.56

1.69

231

0.55

10.95

145.5

42.6

CCZ04522

11

12

1

<0.001

0.0007

0.001

118.5

384

90

6.47

12.3

6.33

3.66

58.3

16.7

2.95

2.2

258

0.92

13.1

158.5

43.4

CCZ04523

12

13

1

<0.001

0.0007

0.001

88.6

292

85

3.63

9.33

5.15

2.71

57.2

12.45

3.51

1.79

202

0.61

12.7

117

32.1

CCZ04524

13

14

1

<0.001

0.0007

0.001

98.8

318

81

5.38

12.6

5.77

4.14

56.9

17.65

2.9

2.28

233

0.68

13.15

145.5

38.3

CCZ04525

14

15

1

<0.001

0.0009

0.001

45.7

486

91

4.58

17.9

6.78

5.7

63

28.4

3.06

2.93

341

0.61

12.45

222

59.1

CCZ04526

15

16

1

<0.001

0.0008

0.001

69.4

577

71

9.24

29

13.5

7.19

61.2

38.1

3.58

5.31

427

1.5

11.4

266

68.9

CCZ04527

16

17

1

0.001

0.0025

0.002

53.4

453

67

5.76

23.3

11.35

5.34

47.1

28

4.04

4.32

322

1.29

10.1

195

50.9

CCZ04528

17

18

1

0.003

0.0017

0.002

118

698

53

17.75

30.3

14.65

7.91

48.2

40.5

1.46

5.72

466

1.5

5.57

303

81.5

CCZ04529

18

19

1

0.045

0.002

0.002

109

774

54

6.11

42.4

16.05

12.35

40.3

60.8

1.61

6.9

644

1.36

6.51

425

106.5

CCZ04530

19

20

1

0.005

0.0011

0.001

193

661

60

2.69

104.5

69.3

15.6

25.8

100

2.98

23.8

597

8.34

7

403

94.2

 























Average







180.0

449.8

74.9

5.4

20.6

10.2

5.7

50.0

27.3

3.2

3.9

308.1

1.1

11.4

211.2

55.9

Source: ALS Adelaide methods ME-MS81 and PGM-MS23 used. Drillhole FG_003RC drilled October 2022.

 



 

FIGURE A7: DRILLHOLE FG_003RC - 0 TO 20M COMPOSITE USED FOR ALS PERTH METALLURGICAL TESTING, 1M ANALYSIS (CONT)

Sample

Number

From

To

Length

ME-MS81

ME-MS81

ME-MS81

ME-MS81

ME-MS81

ME-MS81

ME-MS81

ME-MS81

ME-MS81

ME-MS81

ME-MS81

ME-MS81

ME-MS81

ME-MS81

ME-MS81

ME-MS81

 




Rb

Sc

Sm

Sn

Sr

Ta

Tb

Th

Ti

Tm

U

V

W

Y

Yb

Zr

 

m

m

m

ppm

ppm

ppm

ppm

ppm

ppm

ppm

ppm

%

ppm

ppm

ppm

ppm

ppm

ppm

ppm

CCZ04511

0

1

1

67.5

16.4

10.3

3.2

128

0.9

1.18

12.85

0.49

0.59

4.02

190

3.1

37

3.69

223

CCZ04512

1

2

1

51.2

20

12.35

2.4

180

0.8

1.28

13.65

0.41

0.55

7.54

247

4

35.3

3.39

134

CCZ04513

2

3

1

51.7

19.4

52.8

3.2

126

1

4.53

14.55

0.38

1.18

15.65

191

4.4

76.9

7.01

137

CCZ04514

3

4

1

92.2

37.5

41.8

3.5

129.5

1

3.79

16.3

0.33

0.84

13.85

171

2.8

50.3

5.02

109

CCZ04515

4

5

1

89.1

27.5

38.7

4.3

109.5

1.2

3.52

14.95

0.4

0.78

12.5

178

2.8

53.6

5.09

110

CCZ04516

5

6

1

51.2

14.7

25.9

3.5

91.3

1.1

2.28

16.25

0.38

0.55

7.46

129

3.7

30.9

2.88

100

CCZ04517

6

7

1

78.9

14.7

33.2

2.6

99.1

1

2.98

16.35

0.34

0.57

9.41

106

4.3

35.8

3.23

110

CCZ04518

7

8

1

79.8

11.6

22.6

3.2

101

1.2

1.88

18.25

0.38

0.38

7.65

102

6.3

25.5

2.31

107

CCZ04519

8

9

1

121

16.7

29

3.6

100

1.2

2.58

14.9

0.35

0.71

10.7

140

3

43.1

4.57

99

CCZ04520

9

10

1

160.5

19.6

16.3

3.5

84.7

1.1

1.5

14.3

0.32

0.55

8.74

150

2.2

28.2

4.08

87

CCZ04521

10

11

1

196

20.4

21.6

4.1

89.8

0.9

1.96

14.5

0.31

0.59

12.1

149

1.7

33.6

3.97

87

CCZ04522

11

12

1

171.5

20.2

24

3.7

117

1.1

2.28

19.6

0.34

0.96

15.85

149

3.5

50.9

6.62

99

CCZ04523

12

13

1

108.5

21.4

16.55

3.1

98.9

1.1

1.79

17.65

0.34

0.73

11.2

101

6.3

38.4

4.72

116

CCZ04524

13

14

1

131

20.4

22.3

5

103.5

1

2.28

17.3

0.33

0.79

12.5

136

4

49

4.78

97

CCZ04525

14

15

1

98.8

15.7

35.2

4.3

88.2

1.1

3.64

18.45

0.36

0.81

14.2

170

3.5

57

5

95

CCZ04526

15

16

1

143.5

19.2

41.5

4.3

81.2

1

5.56

18.25

0.31

1.78

20.7

184

2.7

115.5

11.75

113

CCZ04527

16

17

1

84.4

17.6

30.9

3.5

64.9

0.9

4.24

12.7

0.27

1.54

19.1

147

3.6

95.8

9.92

142

CCZ04528

17

18

1

139.5

17.8

47

3.8

51.4

0.4

5.61

6.91

0.15

1.98

38.1

498

4.2

137

12.55

53

CCZ04529

18

19

1

52

38.5

66

5.7

110

0.4

8.47

4.76

0.74

1.94

73.4

580

3

128

11.6

50

CCZ04530

19

20

1

32.7

41.9

72.2

1.5

146

0.4

16

1.57

1.11

9.13

48.7

442

1.1

722

57.8

94

 




















Average




100.1

21.6

33.0

3.6

105.0

0.9

3.9

14.2

0.4

1.3

18.2

208.0

3.5

92.2

8.5

108.1

Source: ALS Adelaide methods ME-MS81 and PGM-MS23 used. Drillhole FG_003RC drilled October 2022.

 


APPENDIX C: REE RESULTS / TREO CONVERSION FACTOR

FIGURE B1: FENCE GOSSAN SURFACE SAMPLING - ALS METHOD ME-MS81 LABORATORY RESULTS

 

HoleID

Sampid

Easting

Northing

from

to

thickness

Th

U

Ce

La

Y

Dy

Er

Eu

Gd

Ho

Lu

Nd

Pr

Sm

Tb

Tm

Yb

TREO  (ppm)

TREO-Ce  (ppm)

LREO  (ppm)

HREO  (ppm)

CREO %

MREO %

MREO_%

FG_SM_T12

CCZ05627

574597.0

6454393.0

0

0.3

0.3

16.0

2.5

113.5

53.6

41.3

7.49

4.33

1.6

8.57

1.49

0.54

49.3

12.95

9.54

1.31

0.59

4.04

373.4

233.9

286.5

86.9

0.33

0.28

27.9

FG_SM_T13

CCZ05628

574601.0

6454194.0

0

0.3

0.3

12.9

2.1

77.7

37.2

36.6

5.95

3.91

1.33

6.33

1.36

0.54

34.9

8.87

6.74

1.03

0.58

3.7

273.2

177.7

198.3

74.9

0.35

0.27

27.3

FG_SM_T14

CCZ05629

574600.0

6453990.0

0

0.3

0.3

14.9

2.2

88.6

43.1

31.1

5.25

3.28

1.11

6.03

1.12

0.46

37.7

10.15

7.22

0.95

0.46

3.05

288.4

179.6

224.0

64.4

0.32

0.27

27.3

FG_SM_T15

CCZ05630

574600.0

6453791.0

0

0.3

0.3

12.8

1.8

73.9

36.2

30.4

5.16

3.17

1.21

6.01

1.09

0.4

33.4

8.87

6.81

0.91

0.48

3.01

254.0

163.3

190.8

63.2

0.34

0.28

28.1

FG_SM_T16

CCZ05631

574599.0

6453588.0

0

0.3

0.3

13.8

1.9

83.5

39.9

32.1

5.65

3.17

1.31

6.31

1.2

0.41

37.7

9.93

7.66

0.99

0.45

2.94

280.8

178.2

214.2

66.5

0.33

0.28

28.4

FG_SM_T17

CCZ05632

574602.0

6453389.0

0

0.3

0.3

14.4

2.0

85.2

41.1

33.3

5.52

3.58

1.19

6.08

1.19

0.55

37.4

9.9

6.89

0.92

0.55

3.7

285.5

180.8

216.4

69.0

0.33

0.27

27.3

FG_SM_T18

CCZ05633

574598.0

6453194.0

0

0.3

0.3

12.1

1.8

84.4

35.7

29

4.93

3.07

1.22

5.79

1.09

0.41

32.2

8.45

6.07

0.92

0.46

2.89

261.0

157.4

200.4

60.7

0.32

0.26

26.1

FG_SM_T19

CCZ05634

574601.0

6452990.0

0

0.3

0.3

13.7

1.9

84.5

41.5

34.6

5.92

3.95

1.34

6.61

1.24

0.48

38.1

9.89

7.45

1.01

0.55

3.64

289.8

186.0

217.5

72.3

0.34

0.28

27.8

FG_SM_T20

CCZ05635

574600.0

6452790.0

0

0.3

0.3

18.3

2.6

104.5

51.5

36.1

6.3

3.94

1.32

7.3

1.31

0.46

46.2

12

9.12

1.06

0.53

3.63

343.3

214.9

267.7

75.5

0.32

0.28

27.9

FG_SM_U12

CCZ05636

574800.0

6454396.0

0

0.3

0.3

17.9

2.4

108.5

51.6

37.6

6.73

3.74

1.49

7.61

1.33

0.51

46.7

12.8

9.28

1.15

0.58

3.54

352.9

219.6

274.5

78.4

0.32

0.28

27.9

FG_SM_U13

CCZ05637

574799.0

6454196.0

0

0.3

0.3

16.6

2.3

98.9

48.7

49.7

8.11

5.28

1.5

9.26

1.82

0.75

46.1

11.95

9.47

1.45

0.8

5.15

360.1

238.6

257.8

102.3

0.36

0.28

28.0

FG_SM_U14

CCZ05638

574802.0

6453995.0

0

0.3

0.3

12.5

2.0

75.1

37.5

42.2

6.24

4.31

1.12

6.31

1.49

0.59

33.9

8.91

6.78

0.99

0.71

4.43

278.0

185.8

194.4

83.6

0.37

0.27

26.5

FG_SM_U15

CCZ05639

574800.0

6453795.0

0

0.3

0.3

14.8

2.3

79.5

37.4

42

6.89

4.58

1.24

6.76

1.57

0.61

35.5

9.28

7.26

1.15

0.71

4.48

288.0

190.4

202.6

85.5

0.37

0.27

27.1

FG_SM_U16

CCZ05640

574803.0

6453599.0

0

0.3

0.3

14.5

2.1

84.8

42.7

37.9

6.2

3.87

1.33

6.34

1.3

0.56

37.9

10.05

7.54

1.06

0.58

3.72

296.1

192.0

219.3

76.8

0.35

0.27

27.3

FG_SM_U17

CCZ05641

574800.0

6453399.0

0

0.3

0.3

14.5

2.2

88.7

44.5

32.5

5.49

3.37

1.23

6.04

1.17

0.49

38.8

10.6

7.47

0.98

0.52

3.1

294.9

185.9

227.9

67.0

0.32

0.28

27.5

FG_SM_U18

CCZ05642

574800.0

6453199.0

0

0.3

0.3

13.4

2.1

78.3

38.8

32.3

5.35

3.28

1.2

5.69

1.09

0.46

35.1

9.27

7.11

0.86

0.45

3.09

267.7

171.6

202.1

65.7

0.34

0.28

27.7

FG_SM_U19

CCZ05643

574799.0

6453000.0

0

0.3

0.3

17.1

2.3

104.5

51

38.2

6.25

3.78

1.44

7.53

1.33

0.6

45.3

12.3

9.02

1.11

0.61

3.63

345.0

216.7

266.3

78.7

0.32

0.28

27.6

FG_SM_U20

CCZ05644

574801.0

6452798.0

0

0.3

0.3

18.4

2.9

105.5

50.5

38.3

6.25

3.97

1.39

7.23

1.35

0.57

45.7

12.2

8.94

1.1

0.57

3.64

345.8

216.2

267.2

78.6

0.32

0.28

27.5

FG_SM_V12

CCZ05645

574999.0

6454394.0

0

0.3

0.3

12.1

1.6

71.3

36.2

27.8

4.74

2.82

1.11

5.23

0.93

0.41

31.8

8.52

6.49

0.83

0.42

2.58

242.2

154.6

185.0

57.2

0.33

0.28

27.8

FG_SM_V13

CCZ05646

575001.0

6454190.0

0

0.3

0.3

15.0

2.2

105

50.3

44.2

7.19

4.65

1.25

7.83

1.55

0.67

45.2

12.1

8.95

1.24

0.66

4.09

355.3

226.3

265.7

89.6

0.34

0.27

27.1

FG_SM_V14

CCZ05647

574999.0

6453995.0

0

0.3

0.3

12.7

1.9

72.8

37.3

38.3

6.21

3.82

1.32

6.08

1.32

0.56

32.9

9.01

6.89

0.99

0.57

3.78

267.4

177.9

190.4

76.9

0.36

0.27

27.1

FG_SM_V15

CCZ05648

574999.0

6453792.0

0

0.3

0.3

15.8

3.3

130.5

64.6

63

10.85

6.35

2.31

11.9

2.23

0.88

62

16.3

13.05

1.84

0.97

5.99

473.0

312.7

343.2

129.8

0.36

0.29

28.6

FG_SM_V16

CCZ05649

575004.0

6453591.0

0

0.3

0.3

16.2

2.7

100

49.9

39.1

6.6

4.1

1.33

7.36

1.37

0.62

43.5

11.6

8.71

1.1

0.61

3.81

336.8

213.9

256.2

80.5

0.33

0.27

27.4

FG_SM_V17

CCZ05650

575000.0

6453393.0

0

0.3

0.3

14.5

2.3

88.5

45.1

36.8

6.15

3.83

1.35

6.56

1.32

0.55

40.8

10.6

7.87

1.02

0.55

3.52

306.4

197.7

231.1

75.3

0.34

0.28

27.9

FG_SM_V18

CCZ05651

575001.0

6453195.0

0

0.3

0.3

14.5

2.4

80

40

31.4

5.28

3.21

1.23

5.69

1.09

0.46

34.6

9.37

7.09

0.9

0.49

3.18

269.7

171.4

205.1

64.6

0.33

0.27

27.3

FG_SM_V19

CCZ05652

574999.0

6452991.0

0

0.3

0.3

13.1

2.2

73.9

36.6

31.2

5.23

3.23

1.04

5.29

1.08

0.49

32

8.7

6.42

0.88

0.49

3.14

252.6

161.8

189.0

63.6

0.34

0.27

27.1

FG_SM_V20

CCZ05653

575001.0

6452793.0

0

0.3

0.3

15.2

2.2

82.2

41.6

34.3

5.31

3.46

1.07

5.99

1.13

0.49

36.5

9.89

7.19

0.86

0.5

3.22

281.5

180.5

212.6

68.9

0.34

0.27

27.3

FG_SM_W12

CCZ05654

575202.0

6454400.0

0

0.3

0.3

16.3

2.3

93.7

45.8

39.4

6.58

4.06

1.37

7.54

1.43

0.57

42.3

11.35

8.53

1.16

0.61

3.97

323.1

208.0

241.8

81.4

0.34

0.28

28.0

FG_SM_W13

CCZ05655

575203.0

6454197.0

0

0.3

0.3

19.5

2.4

91.8

43.7

41.6

6.6

4.21

1.24

7.31

1.43

0.63

39.8

10.8

8.39

1.1

0.64

4.12

317.4

204.6

233.2

84.1

0.35

0.27

27.3

FG_SM_W14

CCZ05656

575203.0

6453997.0

0

0.3

0.3

13.2

2.3

93.2

46.2

40

6.6

4.11

1.41

7.1

1.44

0.58

41.3

11.05

8.3

1.1

0.58

3.75

321.2

206.8

239.8

81.4

0.34

0.27

27.5

FG_SM_W15

CCZ05657

575200.0

6453793.0

0

0.3

0.3

12.5

2.4

106

50.7

49

8.36

4.86

1.79

9.19

1.71

0.71

47.7

12.05

10.15

1.45

0.73

4.46

372.1

241.9

271.6

100.4

0.35

0.28

27.9

FG_SM_W16

CCZ05658

575203.0

6453593.0

0

0.3

0.3

15.8

2.7

102.5

52.5

42.6

6.76

4.16

1.46

7.46

1.4

0.67

44.8

12.2

9.06

1.2

0.67

4.17

351.2

225.3

265.0

86.2

0.33

0.27

27.1

FG_SM_W17

CCZ05659

575198.0

6453396.0

0

0.3

0.3

14.6

2.1

90.2

47.8

30.3

5.44

3.08

1.5

6.4

1.08

0.43

42.7

11.85

8.4

0.94

0.47

2.71

304.5

193.7

240.7

63.8

0.32

0.29

29.1

FG_SM_W18

CCZ05660

575201.0

6453200.0

0

0.3

0.3

15.7

3.0

98.4

52.8

38.7

6.24

4

1.44

7.08

1.36

0.58

43.3

11.8

8.71

1.06

0.61

3.95

337.0

216.2

257.7

79.4

0.33

0.27

27.1

FG_SM_W19

CCZ05661

575204.0

6452996.0

0

0.3

0.3

12.4

1.9

69.2

35.5

34

5.23

3.68

1.21

5.16

1.15

0.61

32.4

8.49

6.17

0.81

0.59

3.75

250.5

165.5

181.8

68.6

0.36

0.27

27.2

FG_SM_W20

CCZ05662

575202.0

6452795.0

0

0.3

0.3

13.7

2.4

58.2

32

28.9

4.49

3.02

0.95

4.72

0.96

0.47

26.4

7.33

5.19

0.7

0.45

3.13

213.1

141.6

154.7

58.4

0.35

0.27

26.8

FG_SM_X12

CCZ05663

575399.0

6454396.0

0

0.3

0.3

19.3

2.3

109

52.7

54.8

8.73

6.03

1.34

8.22

1.9

0.84

45.7

12.4

9.23

1.34

0.92

5.47

384.2

250.3

274.7

109.5

0.35

0.26

26.0

FG_SM_X13

CCZ05664

575400.0

6454192.0

0

0.3

0.3

15.4

3.0

99

48

51.2

8.67

5.28

1.3

8.88

1.83

0.74

44.1

11.7

9.48

1.51

0.81

4.8

358.3

236.7

254.5

103.9

0.36

0.27

27.5

FG_SM_X14

CCZ05665

575402.0

6453996.0

0

0.3

0.3

20.7

3.3

153

82.7

56.1

9.61

5.75

1.85

9.91

2.06

0.86

62.8

17.2

12.25

1.62

0.83

5.35

507.9

319.9

393.2

114.7

0.31

0.26

26.1

FG_SM_X15

CCZ05666

575400.0

6453795.0

0

0.3

0.3

15.6

2.6

98.8

50.4

34.2

5.79

3.24

1.36

6.92

1.18

0.47

42.2

11.35

8.32

1

0.49

3.09

323.5

202.2

253.1

70.5

0.32

0.27

27.3

FG_SM_X16

CCZ05667

575399.0

6453591.0

0

0.3

0.3

15.1

2.8

112.5

59.4

42.4

7.17

4.39

1.72

8.12

1.48

0.62

49.2

13.3

9.16

1.21

0.66

4.07

379.6

241.4

291.9

87.7

0.32

0.27

27.2

FG_SM_X17

CCZ05668

575402.0

6453394.0

0

0.3

0.3

13.7

2.3

98.5

49.7

32.3

5.61

3.28

1.55

6.79

1.16

0.49

43.3

11.75

8.75

1.01

0.47

3.27

322.3

201.3

254.1

68.2

0.31

0.28

28.0

FG_SM_X18

CCZ05669

575404.0

6453192.0

0

0.3

0.3

13.9

2.5

126.5

53.2

45.3

7.54

5

1.95

8.49

1.59

0.76

53.9

13.7

11

1.3

0.74

4.77

404.4

249.0

310.0

94.4

0.33

0.28

27.7

FG_SM_X19

CCZ05670

575398.0

6452993.0

0

0.3

0.3

17.1

2.7

106.5

50.9

37.6

6.32

3.96

1.52

7.16

1.28

0.56

44.9

12.25

8.79

1.07

0.54

3.71

345.6

214.8

267.9

77.7

0.32

0.27

27.2

FG_SM_X20

CCZ05671

575400.0

6452792.0

0

0.3

0.3

14.7

2.5

96.4

47.4

37.4

5.94

3.85

1.5

6.75

1.28

0.58

41.6

11.45

8.28

1.03

0.59

3.64

322.4

203.9

246.0

76.4

0.33

0.27

27.2

FG_SM_Y12

CCZ05672

575600.0

6454397.0

0

0.3

0.3

18.1

2.5

111.5

57.8

45.3

8.02

4.8

1.54

8.88

1.63

0.63

52.8

14.2

10.35

1.36

0.71

4.23

389.5

252.6

295.5

94.0

0.34

0.29

28.7

FG_SM_Y13

CCZ05673

575592.0

6454191.0

0

0.3

0.3

11.1

2.5

102

51.6

42.3

7.62

4.41

1.46

8.1

1.51

0.65

46.3

11.95

9.22

1.26

0.69

4.13

352.9

227.6

264.9

88.0

0.34

0.28

28.0

FG_SM_Y14

CCZ05674

575600.0

6453999.0

0

0.3

0.3

18.3

2.9

125.5

63.1

50.9

8.5

5.34

1.58

8.97

1.79

0.83

52.2

14.55

10.6

1.46

0.78

4.88

422.8

268.6

318.9

103.8

0.33

0.27

26.6

FG_SM_Y15

CCZ05675

575599.0

6453797.0

0

0.3

0.3

14.3

2.7

112

59.1

41.9

6.45

4.12

1.5

7.47

1.36

0.62

49.2

13.3

9.14

1.18

0.62

3.87

375.4

237.8

290.9

84.4

0.32

0.27

27.0

FG_SM_Y16

CCZ05676

575600.0

6453598.0

0

0.3

0.3

16.2

2.6

100.5

52.4

29.2

4.77

2.82

1.26

5.89

0.98

0.4

43.1

12.1

8

0.89

0.45

2.73

319.4

195.9

259.1

60.3

0.30

0.27

27.4

FG_SM_Y17

CCZ05677

575600.0

6453400.0

0

0.3

0.3

12.7

2.2

77.4

40.6

35.4

5.79

3.5

1.33

6.34

1.18

0.49

36.2

9.73

7.52

0.96

0.53

3.45

277.4

182.3

205.4

72.0

0.35

0.28

28.0

FG_SM_Y18

CCZ05678

575598.0

6453200.0

0

0.3

0.3

17.8

2.8

107.5

53.5

36.4

6.05

3.51

1.59

7.03

1.28

0.51

47.6

12.55

8.92

1.08

0.55

3.43

350.8

218.7

275.8

75.0

0.32

0.28

27.7

FG_SM_Y19

CCZ05679

575600.0

6452995.0

0

0.3

0.3

18.4

2.8

105

55.9

40.4

6.74

3.94

1.53

7.72

1.38

0.6

49.9

13.7

9.87

1.14

0.63

3.8

363.6

234.6

280.7

82.9

0.33

0.29

28.7

FG_SM_Y20

CCZ05680

575598.0

6452799.0

0

0.3

0.3

19.3

2.8

115

56

37.4

6.46

3.52

1.33

7.56

1.26

0.52

51.4

13.65

9.9

1.14

0.55

3.27

371.8

230.5

294.9

76.9

0.32

0.28

28.3

FG_SM_Z12

CCZ05681

575795.0

6454397.0

0

0.3

0.3

17.7

2.8

126.5

65.3

61.7

9.72

5.93

1.61

10.45

2.09

0.82

58.5

15.85

11.7

1.71

0.88

5.55

455.8

300.4

332.9

122.9

0.35

0.28

27.7

FG_SM_Z13

CCZ05682

575791.0

6454200.0

0

0.3

0.3

14.1

2.8

113.5

58.9

52.5

8.7

5.3

1.83

9.14

1.89

0.75

52.3

13.75

10.15

1.5

0.82

4.83

404.5

265.1

297.9

106.6

0.35

0.28

27.6

FG_SM_Z14

CCZ05683

575806.0

6453995.0

0

0.3

0.3

14.3

2.0

85.7

43.9

36.2

6.8

3.96

1.48

6.8

1.34

0.5

41.2

11

8.07

1.16

0.59

3.6

303.6

198.3

227.5

76.1

0.35

0.29

28.9

FG_SM_Z15

CCZ05684

575799.0

6453795.0

0

0.3

0.3

13.1

2.9

129

66.4

32.1

5.82

3.12

1.54

7.34

1.11

0.4

51.4

15.1

9.37

1.12

0.43

2.8

393.4

234.9

325.4

68.0

0.28

0.27

26.8

FG_SM_Z16

CCZ05685

575799.0

6453594.0

0

0.3

0.3

12.9

2.5

78.7

39.8

30.8

5.46

3.33

1.33

5.92

1.2

0.46

36.5

9.66

7.18

0.96

0.48

3.1

270.6

173.9

205.9

64.7

0.33

0.28

28.4

FG_SM_Z17

CCZ05686

575797.0

6453396.0

0

0.3

0.3

12.4

2.3

83.3

45.3

44.8

6.7

4.24

1.61

7.39

1.49

0.62

41.2

10.75

8.02

1.18

0.61

3.91

314.6

212.2

225.8

88.8

0.37

0.28

28.0

FG_SM_Z18

CCZ05687

575798.0

6453193.0

0

0.3

0.3

17.2

2.7

111.5

54

49

7.87

5

1.77

8.66

1.69

0.72

48.5

13

9.51

1.33

0.76

4.85

383.3

246.4

283.6

99.7

0.34

0.27

27.1

FG_SM_Z19

CCZ05688

575802.0

6452992.0

0

0.3

0.3

18.1

3.0

108

55.1

45.8

7.17

4.48

1.29

7.39

1.53

0.65

47.6

13.1

8.86

1.26

0.72

4.4

370.2

237.6

278.9

91.3

0.34

0.27

27.0

FG_SM_Z20

CCZ05689

575800.0

6452800.0

0

0.3

0.3

17.3

2.7

118.5

60.5

35.5

6

3.5

1.42

7.06

1.2

0.49

50.2

14.25

9.27

1.07

0.53

3.32

376.4

230.8

303.0

73.3

0.30

0.27

27.3

FG_SM_AA12

CCZ05690

576000.0

6454400.0

0

0.3

0.3

13.0

2.0

86.6

44.2

42.2

6.77

4.39

1.26

7.2

1.49

0.59

40.6

10.5

8.41

1.22

0.64

3.95

313.2

206.8

228.0

85.2

0.36

0.28

27.9

FG_SM_AA13

CCZ05691

576002.0

6454198.0

0

0.3

0.3

13.7

2.0

100.5

54.3

41.8

7.15

4.24

1.64

7.97

1.53

0.59

49.3

13.35

9.68

1.32

0.63

3.93

358.4

234.9

272.0

86.4

0.34

0.29

29.0

FG_SM_AA14

CCZ05692

575997.0

6453998.0

0

0.3

0.3

15.0

2.9

107.5

53.9

36.6

6.55

4.24

1.34

7.24

1.42

0.55

46.4

12.65

9.51

1.18

0.56

4.08

353.4

221.3

275.7

77.7

0.31

0.28

27.6

FG_SM_AA15

CCZ05693

575999.0

6453799.0

0

0.3

0.3

10.4

3.3

130.5

65.2

39.8

7.79

4.09

1.94

8.2

1.51

0.47

57.6

15.4

9.7

1.21

0.66

3.95

418.6

258.3

333.8

84.8

0.31

0.28

27.9

FG_SM_AA16

CCZ05694

576003.0

6453601.0

0

0.3

0.3

13.7

2.1

85

44.6

30.6

5.37

3.05

1.38

6.23

1.06

0.44

38.5

10.5

7.5

0.93

0.46

2.89

286.9

182.5

223.0

63.9

0.32

0.28

28.1

FG_SM_AA17

CCZ05695

575999.0

6453398.0

0

0.3

0.3

12.0

2.1

72.6

38

29.7

5.09

2.99

1.14

5.74

1.04

0.46

33.4

8.92

6.18

0.89

0.44

2.79

252.0

162.8

190.7

61.4

0.34

0.28

27.9

FG_SM_AA18

CCZ05696

575999.0

6453197.0

0

0.3

0.3

15.3

2.6

92.9

48.1

40.7

6.28

3.88

1.33

6.74

1.32

0.63

42.6

11.5

8.04

1.12

0.63

4.03

324.9

210.8

243.4

81.5

0.34

0.27

27.5

FG_SM_AA19

CCZ05697

576006.0

6453003.0

0

0.3

0.3

17.3

2.8

106.5

54.2

33.3

5.53

3.12

1.39

7.01

1.13

0.45

46.4

12.75

8.77

1.07

0.49

2.93

342.9

212.1

274.1

68.9

0.31

0.28

27.8

FG_SM_AA20

CCZ05698

576002.0

6452797.0

0

0.3

0.3

13.4

2.2

84.2

44.4

28.4

4.58

2.85

1.46

5.98

0.94

0.41

38.6

10.65

7.17

0.9

0.42

2.63

280.9

177.5

221.7

59.2

0.32

0.28

28.3

FG_SM_AB12

CCZ05699

576200.0

6454398.0

0

0.3

0.3

17.9

2.6

107.5

54

45.8

7.49

4.82

1.27

8.23

1.52

0.63

49

13.4

9.79

1.36

0.72

4.47

373.3

241.2

280.1

93.2

0.34

0.28

28.0

FG_SM_AB13

CCZ05700

576202.0

6454197.0

0

0.3

0.3

14.8

2.1

91.3

48

37.5

6.21

3.66

1.42

7.19

1.33

0.54

42.5

11.3

8.53

1.1

0.56

3.45

318.4

206.3

241.6

76.9

0.34

0.28

28.2

FG_SM_AB14

CCZ05701

576201.0

6453998.0

0

0.3

0.3

13.8

2.4

105.5

57.5

37.7

6.32

3.64

1.68

7.73

1.29

0.48

48.3

13.15

9.83

1.18

0.53

3.27

358.5

228.9

280.7

77.9

0.32

0.28

28.2

FG_SM_AB15

CCZ05702

576201.0

6453797.0

0

0.3

0.3

11.2

3.4

105

62.5

39.9

6.13

3.61

1.51

7.17

1.28

0.54

45.7

12.75

8.12

1.1

0.54

3.39

360.1

231.1

280.4

79.7

0.32

0.26

26.3

FG_SM_AB16

CCZ05703

576200.0

6453598.0

0

0.3

0.3

14.0

2.5

87.8

45.4

27.4

4.54

2.82

1.2

5.8

0.96

0.4

39

10.7

6.88

0.9

0.45

2.7

285.0

177.1

227.5

57.5

0.31

0.28

27.8

FG_SM_AB17

CCZ05704

576199.0

6453396.0

0

0.3

0.3

12.5

2.2

71.6

37.4

32

5.21

3.4

1.12

5.66

1.09

0.44

33.6

8.73

6.47

0.87

0.46

3.05

254.2

166.2

189.1

65.1

0.35

0.28

27.8

FG_SM_AB18

CCZ05705

576200.0

6453195.0

0

0.3

0.3

18.8

3.2

117.5

60.1

58.4

9.2

5.97

1.63

8.77

1.98

0.92

51.2

14.25

9.62

1.54

0.96

5.71

419.2

274.8

302.9

116.3

0.35

0.26

26.4

FG_SM_AB19

CCZ05706

576200.0

6452999.0

0

0.3

0.3

19.1

3.2

116

59.6

38

6.34

3.74

1.43

7.55

1.28

0.52

50.3

14.1

9.61

1.16

0.58

3.57

377.6

235.1

299.2

78.3

0.31

0.28

27.6

FG_SM_AB20

CCZ05707

576198.0

6452797.0

0

0.3

0.3

18.3

3.2

109.5

56.5

36.6

5.95

3.55

1.43

7.49

1.22

0.52

47.2

12.85

8.51

1.09

0.55

3.5

356.8

222.3

281.2

75.5

0.31

0.27

27.2

FG_SM_AC12

CCZ05708

576403.0

6454399.0

0

0.3

0.3

14.6

2.0

78.2

40.5

34.7

5.59

3.5

1.21

5.74

1.18

0.5

36.2

9.62

7.25

0.95

0.56

3.4

275.9

179.8

205.8

70.0

0.35

0.28

27.7

FG_SM_AC13

CCZ05709

576402.0

6454197.0

0

0.3

0.3

11.2

1.8

89.1

46

31

5.27

3.16

1.63

6.34

1.08

0.43

40.6

11.25

8.08

0.99

0.5

2.87

298.7

189.2

233.7

65.0

0.32

0.28

28.4

FG_SM_AC14

CCZ05710

576402.0

6453998.0

0

0.3

0.3

14.2

2.2

86.4

44.4

30.5

5.04

2.81

1.28

5.56

1.07

0.44

38.9

10.45

7.4

0.88

0.42

2.72

286.7

180.6

224.8

62.0

0.32

0.28

27.8

FG_SM_AC15

CCZ05711

576400.0

6453794.0

0

0.3

0.3

11.8

3.9

143.5

72.2

43.3

7.85

4.42

1.94

9.23

1.61

0.6

60.7

15.65

11.2

1.38

0.63

4.12

455.1

278.9

363.6

91.5

0.30

0.27

27.2

FG_SM_AC16

CCZ05712

576403.0

6453599.0

0

0.3

0.3

16.2

2.6

113

55.1

32.2

5.92

3.02

1.45

6.86

1.17

0.44

48.9

13

8.85

0.99

0.44

2.95

354.0

215.2

286.4

67.6

0.30

0.28

27.9

FG_SM_AC17

CCZ05713

576402.0

6453397.0

0

0.3

0.3

15.8

2.3

101

50.8

36.2

6.39

3.55

1.56

7.35

1.33

0.48

46.8

12.2

8.94

1.09

0.51

3.34

338.7

214.7

263.3

75.4

0.33

0.29

28.6

FG_SM_AC18

CCZ05714

576401.0

6453199.0

0

0.3

0.3

15.7

2.7

102

50.8

44.5

7.27

4.54

1.28

7.67

1.57

0.67

46.5

11.85

8.65

1.16

0.65

4.42

353.5

228.2

263.5

90.1

0.34

0.27

27.5

FG_SM_AC19

CCZ05715

576402.0

6452999.0

0

0.3

0.3

18.9

3.1

116.5

56.5

32.5

6.02

3.33

1.42

7.73

1.2

0.44

51.5

13.9

9.53

1.11

0.44

3.09

367.0

223.9

297.3

69.7

0.30

0.29

28.6

FG_SM_AC20

CCZ05716

576398.0

6452800.0

0

0.3

0.3

20.2

3.7

229

115

38.4

7.22

3.71

2.02

9.82

1.41

0.5

89.7

25.5

14.7

1.4

0.49

3.34

651.8

370.5

568.7

83.1

0.25

0.27

26.7

FG_SM_AD12

CCZ05717

576600.0

6454399.0

0

0.3

0.3

13.3

2.4

93.4

45.4

33.6

5.62

3.4

1.24

6.4

1.25

0.48

40.3

10.5

6.98

0.96

0.5

3.37

305.1

190.4

235.8

69.3

0.32

0.27

27.1

FG_SM_AD13

CCZ05718

576602.0

6454197.0

0

0.3

0.3

11.7

2.0

87.8

44.2

37.8

7.21

4.01

1.62

7.6

1.36

0.48

44.6

11.75

8.29

1.22

0.58

3.58

315.3

207.4

235.5

79.8

0.35

0.30

29.9

FG_SM_AD14

CCZ05719

576601.0

6453992.0

0

0.3

0.3

14.1

2.3

89.4

46

37.3

6.8

4.11

1.7

6.92

1.4

0.57

45

11.7

8.21

1.12

0.59

3.97

318.5

208.7

239.9

78.6

0.35

0.29

29.3

FG_SM_AD15

CCZ05720

576602.0

6453794.0

0

0.3

0.3

12.3

3.9

93

52.4

28.1

5.2

3.25

1.34

6.16

1.06

0.39

40.9

11.2

7.4

0.93

0.46

2.88

306.1

191.9

245.5

60.6

0.30

0.27

27.4

FG_SM_AD16

CCZ05721

576601.0

6453596.0

0

0.3

0.3

15.0

2.7

93

45.2

32.1

6.16

3.42

1.46

6.65

1.26

0.47

43.6

11.5

7.9

1.06

0.48

3.09

309.6

195.3

241.2

68.4

0.33

0.29

29.0

FG_SM_AD17

CCZ05722

576600.0

6453393.0

0

0.3

0.3

17.1

2.9

114

53.6

40.4

7.1

4.41

1.6

7.79

1.38

0.59

50.8

13.4

9.16

1.17

0.59

3.78

372.9

232.9

289.0

83.9

0.33

0.28

28.0

FG_SM_AD18

CCZ05723

576602.0

6453193.0

0

0.3

0.3

20.1

3.3

124.5

61.3

42.1

7.57

4.49

1.58

8.14

1.46

0.61

56.6

15.75

10.35

1.38

0.6

3.94

409.5

256.6

321.9

87.7

0.32

0.29

28.5

FG_SM_AD19

CCZ05724

576599.0

6452995.0

0

0.3

0.3

21.3

3.8

145

70.6

40.8

7.01

3.87

1.61

8.29

1.41

0.52

62.1

16.6

11.4

1.24

0.57

3.85

451.0

272.9

366.6

84.4

0.30

0.28

27.7

FG_SM_AD20

CCZ05725

576600.0

6452793.0

0

0.3

0.3

20.7

3.8

153.5

75.7

41

7.44

4.05

1.77

8.8

1.48

0.59

65.1

17.5

11.25

1.32

0.57

3.67

473.6

285.1

387.5

86.2

0.30

0.28

27.5

FG_SM_AE12

CCZ05726

576799.0

6454395.0

0

0.3

0.3

13.5

1.8

78.4

39.5

30.4

5.28

3.17

1.22

6.08

1.09

0.44

38.1

9.65

6.89

0.87

0.44

3

270.1

173.8

206.7

63.4

0.34

0.29

28.9

FG_SM_AE13

CCZ05727

576803.0

6454195.0

0

0.3

0.3

15.4

2.3

104

51.4

37.5

6.69

3.86

1.52

7.17

1.38

0.51

47.9

12.55

9.12

1.14

0.54

3.49

347.5

219.7

269.6

77.8

0.33

0.28

28.5

FG_SM_AE14

CCZ05728

576803.0

6453996.0

0

0.3

0.3

15.1

2.4

101.5

51.5

34.7

6.15

3.59

1.4

7.13

1.27

0.54

46.3

11.9

8.5

1.09

0.51

3.35

336.1

211.5

263.3

72.8

0.32

0.28

28.2

FG_SM_AE15

CCZ05729

576802.0

6453796.0

0

0.3

0.3

12.4

2.2

78.4

40.3

28.3

4.86

2.88

1.16

5.53

1.01

0.39

35.6

9.42

6.97

0.84

0.42

2.64

263.2

166.9

204.6

58.6

0.32

0.28

28.1

FG_SM_AE16

CCZ05730

576800.0

6453594.0

0

0.3

0.3

14.1

2.7

120

55.6

48.3

7.72

4.79

1.66

7.99

1.76

0.74

52

13.45

9.33

1.3

0.73

4.79

397.8

250.4

300.3

97.5

0.34

0.27

27.0

FG_SM_AE17

CCZ05731

576803.0

6453397.0

0

0.3

0.3

15.1

2.6

119.5

55.8

35.6

6.22

3.66

1.52

7.33

1.29

0.46

52.1

13.55

9.36

1.1

0.49

3.29

374.6

227.8

300.2

74.3

0.31

0.28

28.0

FG_SM_AE18

CCZ05732

576802.0

6453196.0

0

0.3

0.3

22.1

3.4

147

69.4

40.2

7.46

3.9

1.6

8.73

1.42

0.53

62.3

16.6

11.25

1.28

0.56

3.7

452.3

271.7

367.7

84.6

0.30

0.28

27.8

FG_SM_AE19

CCZ05733

576805.0

6453000.0

0

0.3

0.3

20.1

3.5

167

77.4

37.6

6.71

3.65

1.68

8.65

1.4

0.5

68

18.4

11.75

1.26

0.55

3.6

491.0

285.9

411.1

79.9

0.28

0.27

27.4

FG_SM_AE20

CCZ05734

576803.0

6452797.0

0

0.3

0.3

20.9

3.7

134

64.4

48.5

8

4.98

1.55

8.49

1.66

0.76

58.8

15.4

10.15

1.26

0.79

5.08

438.1

273.5

339.1

99.0

0.33

0.27

27.3

FG_SM_AF12

CCZ05735

577004.0

6454394.0

0

0.3

0.3

15.0

2.1

88.3

42.7

38

6.3

3.83

1.2

6.62

1.36

0.53

40.4

10.45

7.3

1.02

0.57

3.83

304.0

195.6

226.8

77.3

0.35

0.28

27.7

FG_SM_AF13

CCZ05736

577002.0

6454198.0

0

0.3

0.3

16.7

2.8

138

64.4

42.6

7.64

4.23

1.67

8.67

1.56

0.66

60.7

16.05

10.9

1.32

0.63

3.9

436.8

267.2

347.9

88.9

0.31

0.28

28.2

FG_SM_AF14

CCZ05737

577001.0

6453993.0

0

0.3

0.3

15.2

2.9

105

51.5

29.8

5.56

3.04

1.26

6.42

1.15

0.41

44.9

11.95

7.82

0.97

0.45

2.77

328.4

199.4

265.3

63.2

0.30

0.28

27.6

FG_SM_AF15

CCZ05738

577001.0

6453795.0

0

0.3

0.3

15.6

2.6

113

57.1

34

6.15

3.24

1.44

7.25

1.18

0.44

51.2

13.5

9.06

1.07

0.45

3.08

363.4

224.6

292.3

71.1

0.31

0.28

28.4

FG_SM_AF16

CCZ05739

577001.0

6453595.0

0

0.3

0.3

16.9

2.7

125.5

61.7

36.8

6.77

3.87

1.66

8.06

1.36

0.46

55.8

14.7

10.05

1.24

0.5

3.42

399.2

245.0

321.0

78.1

0.31

0.28

28.3

FG_SM_AF17

CCZ05740

577003.0

6453394.0

0

0.3

0.3

18.6

3.6

122.5

60

53.5

8.35

5.75

1.37

8.18

1.88

0.82

53.1

14

9.46

1.32

0.87

5.57

417.8

267.3

310.7

107.1

0.34

0.26

26.4

FG_SM_AF18

CCZ05741

577004.0

6453196.0

0

0.3

0.3

20.0

3.2

135

66.3

37.2

6.58

3.71

1.51

8.01

1.35

0.48

59

15.85

10.6

1.22

0.5

3.22

421.6

255.8

343.9

77.8

0.30

0.28

28.1

FG_SM_AF19

CCZ05742

577001.0

6452996.0

0

0.3

0.3

21.8

3.9

146.5

72.1

42.6

7.7

4.28

1.8

9.27

1.55

0.58

64

17.05

12.05

1.33

0.63

4.03

463.6

283.7

373.7

89.9

0.30

0.28

28.1

FG_SM_AF20

CCZ05743

577004.0

6452793.0

0

0.3

0.3

16.9

3.0

106

51.8

33.3

6.01

3.13

1.43

6.8

1.17

0.42

46.6

12.35

8.63

1

0.44

3.03

339.5

209.2

270.2

69.2

0.31

0.28

28.0

FG_SM_AG12

CCZ05744

577200.0

6454399.0

0

0.3

0.3

12.5

2.0

93.3

44.8

41.4

7.32

4.16

1.34

7.5

1.49

0.58

42.9

11.15

8.26

1.2

0.59

3.84

325.0

210.4

240.2

84.8

0.35

0.28

28.2

FG_SM_AG13

CCZ05745

577200.0

6454200.0

0

0.3

0.3

19.0

2.7

106

52.9

37.7

6.73

4.23

1.4

7.36

1.36

0.55

48.9

12.5

9.34

1.26

0.57

3.82

354.4

224.2

275.2

79.2

0.33

0.28

28.4

FG_SM_AG14

CCZ05746

577201.0

6454000.0

0

0.3

0.3

17.9

3.0

123.5

60.3

33.9

5.78

3.42

1.59

7.59

1.26

0.47

53

13.9

9.17

1.12

0.48

3.33

383.5

231.8

311.7

71.8

0.30

0.28

27.6

FG_SM_AG15

CCZ05747

577201.0

6453800.0

0

0.3

0.3

16.7

2.8

112

53.8

35.5

6.35

3.73

1.46

7.36

1.3

0.51

47.3

12.75

9.41

1.14

0.57

3.71

357.3

219.7

282.2

75.1

0.31

0.28

27.6

FG_SM_AG16

CCZ05748

577203.0

6453597.0

0

0.3

0.3

15.6

2.4

101

49

32.4

5.78

3.45

1.27

6.2

1.2

0.47

43.6

11.6

8.09

1.03

0.51

3.23

323.5

199.4

255.8

67.7

0.31

0.28

27.6

FG_SM_AG17

CCZ05749

577202.0

6453396.0

0

0.3

0.3

15.7

2.8

101

50.3

47.5

7.56

5.04

1.53

7.37

1.7

0.71

45

11.95

8.97

1.18

0.76

4.88

356.0

231.9

260.4

95.6

0.35

0.27

26.9

FG_SM_AG18

CCZ05750

577202.0

6453199.0

0

0.3

0.3

15.5

2.9

106

53.2

37.3

6.15

3.85

1.48

6.86

1.32

0.62

45.7

12.15

8.25

1.08

0.6

3.96

347.3

217.1

270.2

77.1

0.32

0.27

27.0

FG_SM_AG19

CCZ05751

577202.0

6452995.0

0

0.3

0.3

19.1

3.3

121

58.9

47.8

7.8

4.7

1.52

7.97

1.6

0.72

51.9

14.1

9.84

1.28

0.72

4.65

402.9

254.3

306.7

96.2

0.33

0.27

27.0

FG_SM_AG20

CCZ05752

577203.0

6452796.0

0

0.3

0.3

17.9

3.3

104.5

50.2

38.9

6.49

3.94

1.37

6.88

1.37

0.62

45.4

11.9

8.61

1.14

0.58

3.79

344.0

215.7

264.6

79.5

0.33

0.27

27.3

FG_SM_AH12

CCZ05753

577402.0

6454398.0

0

0.3

0.3

13.2

1.9

80.5

40

29.1

5.13

3.13

1.28

5.87

1.06

0.44

37

9.63

7.38

0.88

0.45

2.83

270.3

171.4

209.1

61.2

0.33

0.29

28.5

FG_SM_AH13

CCZ05754

577399.0

6454196.0

0

0.3

0.3

14.3

2.7

89.2

43.9

32.5

5.66

3.52

1.31

5.73

1.14

0.47

39.3

10.4

7.56

0.98

0.5

3.41

295.6

186.0

228.2

67.4

0.33

0.28

27.5

FG_SM_AH14

CCZ05755

577399.0

6453998.0

0

0.3

0.3

16.4

2.7

93.3

46.3

28.9

5.21

2.92

1.28

6

1.04

0.39

41.4

10.5

7.77

0.9

0.45

2.69

299.6

185.0

238.9

60.7

0.31

0.28

28.0

FG_SM_AH15

CCZ05756

577400.0

6453799.0

0

0.3

0.3

15.7

3.7

131.5

64.8

37

6.96

3.87

1.75

8.12

1.38

0.52

57.6

15.35

10.4

1.17

0.53

3.41

414.1

252.6

335.3

78.8

0.30

0.28

28.1

FG_SM_AH16

CCZ05757

577397.0

6453596.0

0

0.3

0.3

17.1

2.9

111

55.6

42.8

7.15

4.25

1.6

8.05

1.5

0.66

50.7

13.15

9.63

1.22

0.67

4.37

375.9

239.6

287.8

88.2

0.33

0.28

28.0

FG_SM_AH17

CCZ05758

577401.0

6453397.0

0

0.3

0.3

14.4

2.4

110

54.2

36.7

6.4

3.71

1.53

7.31

1.32

0.53

48.7

12.8

9.22

1.1

0.53

3.48

358.0

222.9

281.7

76.4

0.32

0.28

27.9

FG_SM_AH18

CCZ05759

577402.0

6453194.0

0

0.3

0.3

18.9

3.2

149

70.6

34.4

6.46

3.47

1.69

8.13

1.3

0.46

61.7

16.6

11.2

1.15

0.51

3.18

444.8

261.8

370.8

74.0

0.28

0.28

27.7

FG_SM_AH19

CCZ05760

577398.0

6452998.0

0

0.3

0.3

19.6

3.8

121

58.9

51.7

8.19

5.42

1.56

8.45

1.84

0.84

52.4

13.9

10.55

1.36

0.81

5.43

412.4

263.8

307.9

104.6

0.34

0.27

26.9

FG_SM_AH20

CCZ05761

577395.0

6452801.0

0

0.3

0.3

17.9

2.9

107.5

52.7

38.1

6.63

3.9

1.54

7.3

1.34

0.52

47

12.25

8.94

1.16

0.6

3.78

353.0

220.9

273.8

79.1

0.32

0.28

27.6

FG_SM_AI12

CCZ05762

577600.0

6454397.0

0

0.3

0.3

16.3

2.1

101

49

35.8

6.42

3.8

1.46

6.99

1.34

0.52

45.3

11.8

9.08

1.08

0.58

3.61

334.3

210.2

259.2

75.1

0.32

0.28

28.2

FG_SM_AI13

CCZ05763

577601.0

6454195.0

0

0.3

0.3

16.5

2.7

117.5

64.2

46.1

8.03

4.82

1.69

9.28

1.67

0.76

57.9

15.25

11

1.4

0.73

4.63

414.8

270.5

318.3

96.5

0.33

0.29

29.0

FG_SM_AI14

CCZ05764

577601.0

6453997.0

0

0.3

0.3

16.4

2.8

99.7

48.7

33.6

6.19

3.34

1.35

6.59

1.18

0.49

43.1

11.5

8.36

0.98

0.49

3.54

323.9

201.4

253.4

70.4

0.32

0.28

27.7

FG_SM_AI15

CCZ05765

577603.0

6453799.0

0

0.3

0.3

15.5

3.0

125.5

60.9

34.6

6.23

3.5

1.64

7.49

1.22

0.48

56.5

14.85

10.25

1.12

0.55

3.45

394.8

240.6

321.3

73.4

0.30

0.29

28.6

FG_SM_AI16

CCZ05766

577602.0

6453600.0

0

0.3

0.3

18.7

2.8

108.5

56.2

38.2

6.75

3.89

1.6

7.58

1.42

0.58

51.3

13.6

9.96

1.15

0.61

3.84

367.0

233.7

287.0

80.0

0.33

0.29

28.8

FG_SM_AI17

CCZ05767

577600.0

6453400.0

0

0.3

0.3

17.0

2.7

109.5

53.1

32.8

5.93

3.35

1.52

7.01

1.24

0.51

46.3

12.4

9.23

1.01

0.51

3.32

346.2

211.6

276.5

69.7

0.30

0.28

27.7

FG_SM_AI18

CCZ05768

577599.0

6453198.0

0

0.3

0.3

18.6

3.6

139

67.9

42.5

7.56

4.35

1.67

8.37

1.62

0.63

56.9

15

10.5

1.28

0.63

4.26

435.9

265.2

347.0

88.9

0.30

0.27

26.7

FG_SM_AI19

CCZ05769

577601.0

6452999.0

0

0.3

0.3

14.6

2.3

90.8

45.1

33.9

5.96

3.34

1.33

6.26

1.2

0.47

41.9

10.8

8.2

0.98

0.51

3.4

305.8

194.3

235.9

70.0

0.33

0.28

28.3

FG_SM_AI20

CCZ05770

577602.0

6452799.0

0

0.3

0.3

16.0

2.7

97.8

47.2

34.2

5.84

3.35

1.3

6.31

1.18

0.5

41.9

11.2

8.54

0.98

0.51

3.08

317.7

197.6

247.8

69.9

0.32

0.28

27.5

FG_SM_AJ12

CCZ05771

577802.0

6454397.0

0

0.3

0.3

12.6

2.0

78.9

38.9

33.8

5.67

3.39

1.29

5.94

1.19

0.53

36.9

9.32

7.25

0.94

0.5

3.31

274.3

177.4

205.3

69.1

0.35

0.28

28.1

FG_SM_AJ13

CCZ05772

577802.0

6454194.0

0

0.3

0.3

13.8

2.2

93.2

45.9

32.7

6.14

3.36

1.36

6.75

1.16

0.46

44.2

11.55

8.74

1

0.5

3.29

313.1

198.6

244.0

69.1

0.33

0.29

29.3

FG_SM_AJ14

CCZ05773

577800.0

6454000.0

0

0.3

0.3

14.8

2.9

98.6

50

35

6.17

3.66

1.3

6.43

1.29

0.48

44.3

11.7

8.41

0.99

0.56

3.49

327.8

206.6

255.3

72.4

0.32

0.28

27.8

FG_SM_AJ15

CCZ05774

577802.0

6453794.0

0

0.3

0.3

13.9

2.5

81.6

40.2

31.3

5.21

3.2

1.19

5.8

1.1

0.45

37

9.52

6.72

0.88

0.46

3.14

274.2

174.0

209.8

64.4

0.33

0.28

27.8

FG_SM_AJ16

CCZ05775

577803.0

6453599.0

0

0.3

0.3

14.5

2.5

88.9

44.6

36.4

6.13

3.65

1.32

6.35

1.25

0.57

39.9

10.15

7.7

0.95

0.57

3.85

303.8

194.6

229.2

74.5

0.34

0.27

27.4

FG_SM_AJ17

CCZ05776

577803.0

6453395.0

0

0.3

0.3

14.8

2.3

96.4

47

33

5.82

3.31

1.39

6.5

1.2

0.44

42.4

11

8.65

1.05

0.5

3.26

315.2

196.8

246.3

68.9

0.32

0.28

28.0

FG_SM_AJ18

CCZ05777

577803.0

6453196.0

0

0.3

0.3

18.7

3.1

132.5

64.1

35.3

6.35

3.33

1.52

7.66

1.26

0.46

56

15.05

10.3

1.12

0.55

3.26

407.5

244.8

333.4

74.1

0.30

0.28

27.7

FG_SM_AJ19

CCZ05778

577804.0

6452998.0

0

0.3

0.3

15.4

2.6

97.9

46.9

36.8

6.15

3.87

1.35

6.76

1.26

0.63

42.8

11.1

7.96

1.06

0.61

3.84

323.9

203.6

247.8

76.0

0.33

0.27

27.4

FG_SM_AJ20

CCZ05779

577806.0

6452797.0

0

0.3

0.3

19.0

2.7

109

52.8

35.3

6.32

3.35

1.48

7.78

1.26

0.52

48.7

12.7

9.08

1.08

0.49

3.26

352.7

218.8

278.5

74.2

0.32

0.28

28.4

FG_SM_AK12

CCZ05780

577999.0

6454401.0

0

0.3

0.3

15.1

2.5

89.1

43.1

34.2

5.45

3.5

1.28

6.25

1.21

0.51

40.5

10.8

8.19

0.93

0.5

3.46

299.7

190.3

229.8

69.9

0.33

0.28

28.1

FG_SM_AK13

CCZ05781

578003.0

6454202.0

0

0.3

0.3

12.2

2.1

76.3

37.2

29.2

5.03

2.85

1.3

5.37

1.01

0.45

34.7

9.07

7.09

0.86

0.45

2.97

257.4

163.7

197.0

60.4

0.33

0.28

28.2

FG_SM_AK14

CCZ05782

578000.0

6454000.0

0

0.3

0.3

14.0

2.6

94.4

46

42.1

6.87

4.39

1.4

6.2

1.49

0.69

41.3

10.95

7.87

1.08

0.67

4.71

325.5

209.5

240.4

85.0

0.35

0.27

26.7

FG_SM_AK15

CCZ05783

578003.0

6453798.0

0

0.3

0.3

14.9

2.4

96.6

47.6

34.8

6.12

3.56

1.52

6.82

1.25

0.57

43.5

11.6

8.91

1.04

0.51

3.39

322.2

203.6

249.6

72.7

0.33

0.28

28.3

FG_SM_AK16

CCZ05784

578001.0

6453601.0

0

0.3

0.3

14.9

2.4

99.5

48.8

37

6.11

3.69

1.48

6.92

1.27

0.54

44.1

11.9

8.58

1.06

0.55

3.53

331.1

208.9

255.2

75.9

0.33

0.28

27.8

FG_SM_AK17

CCZ05785

578003.0

6453400.0

0

0.3

0.3

14.8

2.4

90.3

44.7

35.8

5.99

3.79

1.5

6.32

1.29

0.6

40.6

10.75

7.96

0.97

0.57

3.98

307.1

196.2

232.9

74.2

0.33

0.28

27.6

FG_SM_AK18

CCZ05786

578001.0

6453200.0

0

0.3

0.3

16.7

2.8

105.5

54.8

37.9

6.53

3.83

1.45

6.98

1.32

0.59

45.5

12.2

8.79

1.06

0.56

3.87

350.1

220.5

271.9

78.2

0.32

0.27

27.1

FG_SM_AK19

CCZ05787

578003.0

6452998.0

0

0.3

0.3

16.6

2.5

102.5

49.2

34.9

6.03

3.59

1.42

7.02

1.27

0.46

46

12.3

8.74

1.02

0.48

3.33

334.9

209.0

262.3

72.6

0.32

0.28

28.3

FG_SM_AK20

CCZ05788

578003.0

6452793.0

0

0.3

0.3

19.2

3.0

127.5

61.5

36.4

6.41

3.46

1.84

8.02

1.28

0.48

58.3

15.7

10.95

1.2

0.48

3.32

405.1

248.5

328.4

76.7

0.31

0.29

29.1

FG_SM_AL12

CCZ05789

578197.0

6454400.0

0

0.3

0.3

14.4

2.0

84.5

42

31.5

5.59

3.19

1.43

6.39

1.17

0.45

38.5

10.2

7.81

0.96

0.47

3.08

285.5

181.7

219.3

66.1

0.33

0.28

28.4

FG_SM_AL13

CCZ05790

578199.0

6454196.0

0

0.3

0.3

11.6

1.9

74.2

38

31.9

4.89

3.09

1.28

5.46

1.06

0.48

34.2

8.88

6.49

0.85

0.44

3.02

258.0

166.8

193.9

64.1

0.34

0.28

27.5

FG_SM_AL14

CCZ05791

578199.0

6453998.0

0

0.3

0.3

12.6

2.1

86.3

42.5

33.8

5.73

3.48

1.34

6.02

1.22

0.49

39.9

10.65

7.84

0.99

0.49

3.53

294.0

188.0

224.4

69.7

0.34

0.28

28.3

FG_SM_AL15

CCZ05792

578199.0

6453798.0

0

0.3

0.3

15.0

2.3

121.5

63.4

33.6

5.58

3.26

1.5

6.53

1.14

0.47

51.9

14.9

8.81

0.98

0.48

3.21

381.6

232.4

312.4

69.3

0.29

0.27

27.2

FG_SM_AL16

CCZ05793

578200.0

6453600.0

0

0.3

0.3

13.2

2.7

107

55.9

33.4

5.83

3.31

1.46

7

1.19

0.47

47.4

13.1

8.9

1.03

0.48

3.22

348.4

217.0

278.4

70.0

0.31

0.28

28.0

FG_SM_AL17

CCZ05794

578200.0

6453400.0

0

0.3

0.3

20.1

3.3

137.5

66.9

39.3

7.07

4.07

1.83

8.71

1.44

0.55

62

16.95

11.85

1.22

0.56

3.56

437.1

268.2

353.9

83.2

0.31

0.29

28.9

FG_SM_AL18

CCZ05795

578198.0

6453200.0

0

0.3

0.3

21.6

3.5

130.5

62.6

44

7.35

4.67

1.63

8.11

1.51

0.72

57.9

15.4

10.75

1.22

0.69

4.59

423.2

262.9

332.3

90.9

0.32

0.28

27.8

FG_SM_AL19

CCZ05796

578202.0

6452996.0

0

0.3

0.3

16.5

2.5

97.6

50.1

42.7

6.97

4.4

1.62

7.35

1.48

0.64

46.6

11.95

9.15

1.2

0.63

4.2

345.0

225.1

258.1

86.9

0.35

0.28

28.2

FG_SM_AL20

CCZ05797

578206.0

6452796.0

0

0.3

0.3

18.4

3.4

125.5

59.4

33.7

5.89

3.37

1.42

6.8

1.18

0.52

51.5

14.1

9.62

1.03

0.52

3.39

382.6

228.4

312.1

70.5

0.29

0.27

27.2

FG_SM_AM12

CCZ05798

578401.0

6454397.0

0

0.3

0.3

14.3

2.3

91.7

45.1

35

5.9

3.43

1.44

6.43

1.18

0.52

41.8

11.05

8

0.97

0.52

3.44

308.7

196.1

236.9

71.8

0.33

0.28

28.1

FG_SM_AM13

CCZ05799

578398.0

6454195.0

0

0.3

0.3

13.4

1.9

74.9

37

28.8

4.96

2.98

1.35

5.42

1.01

0.42

34.4

9.21

7.06

0.86

0.43

3

254.9

162.9

194.8

60.0

0.33

0.28

28.4

FG_SM_AM14

CCZ05800

578402.0

6453997.0

0

0.3

0.3

16.9

2.1

90.1

42.7

33.7

5.48

3.28

1.24

5.89

1.14

0.45

40.9

10.65

8.18

0.92

0.42

3.12

298.8

188.1

230.8

68.0

0.33

0.28

28.2

FG_SM_AM15

CCZ05801

578400.0

6453800.0

0

0.3

0.3

13.7

2.3

117

57

41.3

6.92

4

1.44

7.23

1.43

0.55

47.7

12.9

9.4

1.15

0.58

3.99

376.5

232.8

292.7

83.8

0.32

0.26

26.5

FG_SM_AM16

CCZ05802

578401.0

6453596.0

0

0.3

0.3

22.6

3.6

115

56.6

31.1

5.8

3.28

1.22

6.9

1.15

0.46

48.4

13.55

9.59

1.06

0.46

3.14

358.0

216.8

291.6

66.5

0.29

0.28

27.9

FG_SM_AM17

CCZ05803

578402.0

6453395.0

0

0.3

0.3

12.3

2.6

82.5

40.1

29.7

5.05

2.97

1.19

5.54

1.1

0.47

36.3

9.76

7.47

0.84

0.46

2.98

272.5

171.2

211.2

61.4

0.32

0.28

27.9

FG_SM_AM18

CCZ05804

578398.0

6453196.0

0

0.3

0.3

16.4

3.5

106

53.1

41.4

7.04

4.2

1.7

7.76

1.47

0.62

49.9

12.95

9.76

1.2

0.61

3.82

362.9

232.7

277.7

85.2

0.34

0.29

28.6

FG_SM_AM19

CCZ05805

578400.0

6452994.0

0

0.3

0.3

14.9

3.1

96.6

48.1

34.7

5.77

3.49

1.35

6.24

1.21

0.5

43.3

11.25

8.36

1.02

0.53

3.3

319.8

201.2

248.9

71.0

0.33

0.28

27.8

FG_SM_AM20

CCZ05806

578402.0

6452797.0

0

0.3

0.3

16.6

2.6

99.9

53

37.1

6

3.63

1.5

7.02

1.29

0.51

45

12.15

8.79

1.08

0.49

3.37

337.9

215.2

262.2

75.7

0.32

0.28

27.7

FG_SM_AN12

CCZ05807

578598.0

6454396.0

0

0.3

0.3

13.9

2.2

76.5

37.8

36.7

5.74

3.64

1.16

6.03

1.27

0.59

35.5

9.45

7.17

0.95

0.56

3.72

273.2

179.2

199.4

73.8

0.36

0.28

27.7

FG_SM_AN13

CCZ05808

578600.0

6454197.0

0

0.3

0.3

15.2

2.3

84.9

43

37.1

6.28

3.82

1.22

6.42

1.35

0.57

40.3

10.6

7.92

0.99

0.57

3.97

299.8

195.5

223.7

76.0

0.35

0.28

28.3

FG_SM_AN14

CCZ05809

578600.0

6453994.0

0

0.3

0.3

16.9

3.0

113

58.1

51

8.69

5.24

1.28

8.76

1.82

0.75

53.6

14.2

10.2

1.36

0.78

5.27

402.2

263.4

298.5

103.7

0.35

0.28

28.1

FG_SM_AN15

CCZ05810

578599.0

6453795.0

0

0.3

0.3

19.5

5.5

113.5

55.4

43.2

7.4

4.41

1.47

7.3

1.47

0.73

49

12.95

9.25

1.19

0.71

4.8

376.6

237.2

287.9

88.7

0.33

0.27

27.0

FG_SM_AN16

CCZ05811

578599.0

6453597.0

0

0.3

0.3

13.3

2.8

100.5

49.8

31.7

5.53

3.12

1.32

6.13

1.08

0.52

44

11.85

8.22

0.95

0.45

3.34

323.1

199.6

257.0

66.0

0.31

0.28

27.8

FG_SM_AN17

CCZ05812

578600.0

6453397.0

0

0.3

0.3

13.5

2.6

94

44.6

37.6

6.16

3.54

1.58

7.17

1.35

0.54

42.3

10.85

8.36

1.06

0.59

3.81

317.3

201.8

239.9

77.4

0.34

0.28

28.0

FG_SM_AN18

CCZ05813

578603.0

6453197.0

0

0.3

0.3

14.2

2.4

87

42.6

34.8

5.73

3.57

1.2

6.32

1.22

0.54

39.2

10.35

7.64

0.99

0.54

3.42

295.1

188.3

223.9

71.2

0.34

0.28

27.8

FG_SM_AN19

CCZ05814

578599.0

6452996.0

0

0.3

0.3

15.2

3.3

104

51.5

38.7

6.83

4.15

1.64

7.36

1.44

0.55

46.9

12.55

9.19

1.18

0.58

3.59

349.2

221.4

268.7

80.5

0.33

0.28

28.1

FG_SM_AN20

CCZ05815

578600.0

6452794.0

0

0.3

0.3

16.9

3.0

99.3

50.4

38.9

6.37

4.14

1.46

7.01

1.42

0.57

46

12.35

8.75

1.14

0.62

3.75

339.6

217.6

259.8

79.8

0.33

0.28

28.1

FG_SM_V22

CCZ05816

574999.0

6452396.0

0

0.3

0.3

15.9

2.3

95.6

46.8

32.9

5.6

3.69

1.25

6.19

1.17

0.47

45.5

11.35

8.64

0.93

0.55

2.95

317.1

199.7

249.1

68.0

0.33

0.29

28.8

FG_SM_V24

CCZ05817

575004.0

6451998.0

0

0.3

0.3

19.3

2.8

104

50.8

30.7

5.76

3.46

1.34

6.99

1.15

0.44

47.8

12

9.51

1.04

0.42

2.64

334.3

206.5

268.6

65.7

0.31

0.29

29.1

FG_SM_V26

CCZ05818

575000.0

6451593.0

0

0.3

0.3

12.9

1.9

65.3

33.9

23.7

4.3

2.71

0.91

4.61

0.89

0.37

32.1

7.83

6.3

0.71

0.37

2.31

224.0

143.8

174.2

49.8

0.33

0.29

29.1

FG_SM_V28

CCZ05819

574997.0

6451196.0

0

0.3

0.3

14.2

2.2

77.7

39.1

32.1

5.26

3.59

1.14

5.92

1.16

0.53

38.6

9.68

7.32

0.89

0.55

3.13

272.7

177.3

206.5

66.2

0.35

0.29

29.0

FG_SM_V30

CCZ05820

575000.0

6450798.0

0

0.3

0.3

12.8

1.9

71.5

35.7

27.9

4.76

3.18

1.12

5.29

1.02

0.44

35

8.7

6.8

0.79

0.44

2.79

247.1

159.3

188.9

58.2

0.34

0.29

29.0

FG_SM_X22

CCZ05821

575400.0

6452404.0

0

0.3

0.3

14.9

2.4

99.5

46.8

28.5

5.07

3.07

1.56

6.69

1.03

0.38

46.6

11.7

9.41

0.93

0.4

2.41

317.5

195.2

256.5

60.9

0.31

0.30

29.6

FG_SM_X24

CCZ05822

575401.0

6452002.0

0

0.3

0.3

16.4

1.9

65.9

33.5

26

4.08

2.73

1.01

5.02

0.94

0.39

32.6

8

6.02

0.76

0.36

2.36

228.2

147.3

174.9

53.3

0.34

0.29

28.9

FG_SM_X26

CCZ05823

575398.0

6451601.0

0

0.3

0.3

15.6

2.6

112

50.7

35.2

6.31

4.16

1.68

7.48

1.37

0.53

51.2

13.2

9.88

1.11

0.59

3.22

359.3

221.7

284.2

75.1

0.32

0.29

29.0

FG_SM_X28

CCZ05824

575404.0

6451203.0

0

0.3

0.3

17.5

2.9

97.4

46.5

33.8

5.53

3.97

1.16

6.63

1.26

0.54

44

11.5

8.69

0.99

0.51

3.46

320.0

200.4

249.5

70.5

0.32

0.28

28.3

FG_SM_X30

CCZ05825

575398.0

6450803.0

0

0.3

0.3

15.4

2.4

77.4

37.5

31.4

5.02

3.39

1.04

5.51

1.06

0.45

36

9.23

6.81

0.87

0.48

2.88

263.7

168.7

200.1

63.6

0.34

0.28

28.1

FG_SM_Z22

CCZ05826

575800.0

6452401.0

0

0.3

0.3

17.0

2.8

101

48.3

30.1

5.37

3.15

1.25

6.53

1.14

0.43

45.6

11.75

9.2

0.97

0.43

2.76

322.3

198.2

258.8

63.5

0.31

0.29

28.8

FG_SM_Z24

CCZ05827

575803.0

6451997.0

0

0.3

0.3

14.6

2.3

100

48.8

29.9

5.33

3.53

1.5

6.65

1.12

0.42

47.2

12.35

9.19

0.94

0.44

2.64

324.6

201.8

260.7

63.9

0.31

0.29

29.4

FG_SM_Z26

CCZ05828

575798.0

6451599.0

0

0.3

0.3

17.2

2.8

100.5

47.7

36.9

6.12

4.45

1.28

6.65

1.38

0.59

46.4

11.75

8.64

1.03

0.57

3.63

334.1

210.6

257.7

76.4

0.33

0.28

28.2

FG_SM_Z28

CCZ05829

575801.0

6451202.0

0

0.3

0.3

15.7

2.4

91.7

45.4

34

5.77

3.97

1.2

6.48

1.2

0.5

45

11.25

8.5

0.97

0.51

3.35

312.5

199.9

241.8

70.7

0.34

0.29

29.2

FG_SM_Z30

CCZ05830

575802.0

6450799.0

0

0.3

0.3

15.3

2.4

80.9

41.4

33.2

5.66

3.83

1.3

6.33

1.24

0.49

40.3

10

7.73

0.98

0.51

3.41

285.4

186.0

216.0

69.4

0.34

0.29

29.1

FG_SM_AB22

CCZ05831

576199.0

6452399.0

0

0.3

0.3

13.0

2.4

82.9

41.2

28

5

3.17

1.41

5.57

0.97

0.33

38.6

9.6

7.18

0.8

0.41

2.45

273.8

171.9

215.1

58.7

0.32

0.29

28.5

FG_SM_AB24

CCZ05832

576198.0

6451999.0

0

0.3

0.3

18.0

3.1

108

50.8

34.6

6.03

3.64

1.4

6.95

1.2

0.51

48

12.2

9.16

1.07

0.49

3.33

345.8

213.1

273.6

72.2

0.32

0.28

28.2

FG_SM_AB26

CCZ05833

576201.0

6451598.0

0

0.3

0.3

16.8

2.5

96.5

49.3

33.3

5.83

3.78

1.32

6.93

1.2

0.51

48.7

12.1

8.73

1

0.53

2.99

327.9

209.3

257.9

70.0

0.33

0.30

29.7

FG_SM_AB28

CCZ05834

576201.0

6451197.0

0

0.3

0.3

15.6

2.6

106.5

50.7

32.6

5.7

3.71

1.51

6.67

1.18

0.43

49.6

12.35

9.57

1.03

0.49

2.94

342.7

211.9

274.2

68.6

0.32

0.29

29.0

FG_SM_AB30

CCZ05835

576201.0

6450798.0

0

0.3

0.3

12.4

1.9

66.5

32

29.4

4.62

3.41

1.12

5.22

1.02

0.39

33.1

7.8

6.39

0.86

0.46

2.71

234.7

153.1

174.7

60.1

0.36

0.29

28.9

FG_SM_POC

CCZ05836

575129.0

6451468.0

0

0.3

0.3

18.0

2.9

103.5

52.2

36.1

5.57

4.15

1.5

7.31

1.28

0.6

49.9

12.8

9.52

1.06

0.61

3.64

348.4

221.3

273.1

75.4

0.33

0.29

28.9

Notes:

1.                Verification has been undertaken by CCZ Geology team personnel.

2.                Sample results from ALS method ME-ICP81.

Source: ALS Adelaide.


APPENDIX D: JORC CODE, 2012 EDITION - TABLE 1 - FENCE GOSSAN SURFACE SAMPLING

Section 1: Sampling Techniques and Data

Criteria

JORC Code explanation

Commentary

Sampling techniques

Nature and quality of sampling (e.g., cut channels, random chips, or specific specialised industry standard measurement tools appropriate to the minerals under investigation, such as down hole gamma sondes, or handheld XRF instruments, etc.). These examples should not be taken as limiting the broad meaning of sampling.

Include reference to measures taken to ensure sample representivity and the appropriate calibration of any measurement tools or systems used.

Aspects of the determination of mineralisation that are Material to the Public Report.

In cases where 'industry standard' work has been done this would be relatively simple (e.g., 'reverse circulation drilling was used to obtain 1 m samples from which 3 kg was pulverised to produce a 30g charge for fire assay'). In other cases, more explanation may be required, such as where there is coarse gold that has inherent sampling problems. Unusual commodities or mineralisation types (eg submarine nodules) may warrant disclosure of detailed information.

Diamond Drilling (DDH)

Diamond drilling of HQ diameter (TT_005DD) was completed to 137.7m recently in the completed program and was located 5m away from a RC hole already drilled (TT_003RC).

Reverse Circulation ('RC') Drilling

RC drilling at Fence Gossan was used to obtain a representative sample by means of riffle splitting with samples submitted for analysis using the above-mentioned methodologies.

Four (4) reverse circulation (RC) holes for a total of 516m have been completed at the Fence Gossan Prospect.

Four (4) RC holes were completed at Reefs Tank for a total of 564m.

At Tors Tank, four (4) RC holes for a total of 625.7m (including the cored hole) were completed.

The RC drilling technique was used to obtain a representative sample by means of a cone or riffle splitter with samples submitted for assay by mixed acid digestion and analysis via ICP-MS + ICP-AES with anticipated reporting a suite of 48 elements (sulphur >10% by LECO)

Surface Sampling

Two large surface sampling programs were conducted on grids based about the drilling at Tors Tank and Fence Gossan.  The sampling was by using hand auger to take soil samples from depth varying between 0.1-0.5m.  Original samples were between 0.5-2kg in weight, reduced to 200g for crushing and pulverizing.  The Stage 1 program consisted of 189 sampling stations, spaced at 200m intervals across a total survey area measuring 6.4km2

The first area was based about the centre of the grid, closest to the known points of observations (drill holes FG001RC-4RC).  Stations extended east of the Resource Mask to the EL8434 lease boundary.  Stations also extended west to identify extension of REEs into the Reef Tank Resource Area.  Station numbers are based on a wider grid that incorporates Reef Tank and Tors Tank.

A Stage 2 second area at a larger spacing (400m) was completed slighter later in December 2022, which managed to collect another 21 samples over mainly pegmatite outcrop.

Drilling techniques

Drill type (e.g., core, reverse circulation, open-hole hammer, rotary air blast, auger, Bangka, sonic, etc.) and details (e.g., core diameter, triple or standard tube, depth of diamond tails, face-sampling bit or other type, whether core is oriented and if so, by what method, etc.).

Historical drilling consisted of auger, rotary air blast, reverse circulation, and NQ, BQ, and HQ diamond coring.  One cored hole of HQ (61mm) diameter was completed at Tors Tank after all the RC holes had been completed.

Diamond drilling was completed with standard diameter, conventional HQ, with historical holes typically utilizing RC and percussion pre-collars to an average 30 metres (see drillhole information for further details).

Drill sample recovery

Method of recording and assessing core and chip sample recoveries and results assessed.

Measures taken to maximise sample recovery and ensure representative nature of the samples.

Whether a relationship exists between sample recovery and grade and whether sample bias may have occurred due to preferential loss/gain of fine/coarse material.

Reverse Circulation ('RC') Drilling - Reverse circulation sample recoveries were visually estimated during drilling programs. Where the estimated sample recovery was below 100% this was recorded in field logs by means of qualitative observation.

Reverse circulation drilling employed sufficient air (using a compressor and booster) to maximise sample recovery.  Historical cored drillholes by North Broken Hill, CRA , and Pasminco were well documented and generally have >90% core recovery.

No relationship between sample recovery and grade has been observed.

Logging

Whether core and chip samples have been geologically and geotechnically logged to a level of detail to support appropriate Mineral Resource estimation, mining studies and metallurgical studies.

Whether logging is qualitative or quantitative in nature. Core (or costean, channel, etc) photography.

The total length and percentage of the relevant intersections logged.

The drilling that did occur was completed to modern-day standards. The preferred exploration strategy in the eighties and early nineties was to drill shallow auger holes to negate the influence of any Quaternary and Tertiary sedimentary cover, and then return to sites where anomalous Cu or Zn were assayed.  In this program at all three areas holes were completed to varying depths ranging from 100-160m.

No downhole geophysical logging took place; however, measurements of magnetic susceptibility were taken at the same 1m intervals as the PXRF readings were taken.

Sub-sampling techniques and sample preparation

If core, whether cut or sawn and whether quarter, half or all core taken.

If non-core, whether riffled, tube sampled, rotary split, etc and whether sampled wet or dry.

For all sample types, the nature, quality, and appropriateness of the sample preparation technique.

Quality control procedures adopted for all sub-sampling stages to maximise representivity of samples.

Measures taken to ensure that the sampling is representative of the in-situ material collected, including for instance results for field duplicate/second-half sampling.

Whether sample sizes are appropriate to the grain size of the material being sampled.

Core samples will be hand-split or sawn with re-logging of available historical core indicating a 70:30 (retained: assayed) split was typical. The variation of sample ratios noted are considered consistent with the sub-sampling technique (hand-splitting).

No second half samples will be submitted for analysis, but duplicates have been taken at a frequency of 1:20 in samples collected.

It is considered water planned to be used for core cutting is unprocessed and unlikely to have introduced sample contamination.

Procedures relating to the definition of the line of cutting or splitting are not available.  It is expected that 'standard industry practice' for the period was applied to maximize sample representivity.

Quarter core will be submitted to ALS for chemical analysis using industry standard sample preparation and analytical techniques.

The sample interval details and grades quoted for cored intervals described in various maps in the main section are given in previous ASX releases (Castillo Copper 2022a, b, c, d, e, f, g).

Quality of assay data and laboratory tests

The nature, quality and appropriateness of the assaying and laboratory procedures used and whether the technique is considered partial or total.

For geophysical tools, spectrometers, handheld XRF instruments, etc, the parameters used in determining the analysis including instrument make and model, reading times, calibrations factors applied and their derivation, etc.

Nature of quality control procedures adopted (eg standards, blanks, duplicates, external laboratory checks) and whether acceptable levels of accuracy (i.e. lack of bias) and precision have been established.

 

The following rare earth elements were analysed using ME-MS61R Sample Decomposition is by HF-HNO3-HClO4 acid digestion, HCl leach (GEO-4A01).  The Analytical Method for

Silver is shown below:

Element

Symbol

Units

Lower Limit

Upper Limit

Silver

Ag

ppm

0.01

100

Inductively Coupled Plasma - Atomic Emission Spectroscopy (ICP - AES) Inductively Coupled Plasma - Mass Spectrometry (ICP-MS)

A prepared sample (0.25 g) is digested with perchloric, nitric, hydrofluoric, and hydrochloric acids. The residue is topped up with dilute hydrochloric acid and analysed by inductively coupled plasma atomic emission spectrometry. Following this analysis, the results are reviewed for high concentrations of bismuth, mercury, molybdenum, silver, and tungsten and diluted accordingly.

Samples meeting this criterion are then analysed by inductively coupled plasma-mass spectrometry. Results are corrected for spectral interelement interferences.

Four acid digestions can dissolve most minerals: however, although the term "near total" is used, depending on the sample matrix, not all elements are quantitatively extracted.

Results for the additional rare earth elements will represent the acid leachable portion of the rare earth elements and as such, cannot be used, for instance to do a chondrite plot.

Geochemical Procedure

Element geochemical procedure reporting units and limits are listed below:

Element

Symbol

Units

Lower Limit

Upper Limit

Aluminum

Al

%

0.01

50

Arsenic

As

ppm

0.2

10 000

Barium

Ba

ppm

10

10 000

Beryllium

Be

ppm

0.05

1 000

Bismuth

Bi

ppm

0.01

10 000

Calcium

Ca

%

0.01

50

Cadmium

Cd

ppm

0.02

1 000

Cerium

Ce

ppm

0.01

500

Cobalt

Co

ppm

0.1

10 000

Chromium

Cr

ppm

1

10 000

Cesium

Cs

ppm

0.05

500

Copper

Cu

ppm

0.2

10 000

Iron

Fe

%

0.01

50

Gallium

Ga

ppm

0.05

10 000

Germanium

Ge

ppm

0.05

500

Hafnium

Hf

ppm

0.1

500

Indium

In

ppm

0.005

500

Potassium

K

%

0.01

10

Lanthanum

La

ppm

0.5

10 000

Lithium

Li

ppm

0.2

10 000

Magnesium

Mg

%

0.01

50

Manganese

Mn

ppm

5

100 000

 

Element

Symbol

Units

Lower Limit

Upper Limit

Molybdenum

Mo

ppm

0.05

10 000

Sodium

Na

%

0.01

10

Niobium

Nb

ppm

0.1

500

Nickel

Ni

ppm

0.2

10 000

Phosphorous

P

ppm

10

10 000

Lead

Pb

ppm

0.5

10 000

Rubidium

Rb

ppm

0.1

10 000

Rhenium

Re

ppm

0.002

50

Sulphur

S

%

0.01

10

Antimony

Sb

ppm

0.05

10 000

Scandium

Sc

ppm

0.1

10 000

Selenium

Se

ppm

1

1 000

Tin

Sn

ppm

0.2

500

Strontium

Sr

ppm

0.2

10 000

Tantalum

Ta

ppm

0.05

100

Tellurium

Te

ppm

0.05

500

Thorium

Th

ppm

0.2

10 000

Titanium

Ti

%

0.005

10

Thallium

Tl

ppm

0.02

10 000

Uranium

U

ppm

0.1

10 000

Vanadium

V

ppm

1

10 000

Tungsten

W

ppm

0.1

10 000

Method ME-MS81

This method involves a lithium borate fusion prior to acid dissolution and ICP- MS analysis provides the most quantitative analytical approach for a broad suite of trace elements.  Options for adding the whole rock elements from an |CP - AES analysis on the same fusion, or base metals from a separate four acid digestion, are available.

Lower and upper detection limits are given below:

Element

Symbol

Units

Lower Limit

Upper Limit

Yttrium

Y

ppm

0.1

500

Zinc

Zn

ppm

2

10 000

Zirconium

Zr

ppm

0.5

500

Dysprosium

Dy

ppm

0.05

1 000

Erbium

Er

ppm

0.03

1 000

Europium

Eu

ppm

0.03

1 000

Gadolinium

Gd

ppm

0.05

1 000

Holmium

Ho

ppm

0.01

1 000

Lutetium

Lu

ppm

0.01

1 000

Neodymium

Nd

ppm

0.1

1 000

Praseodymium

Pr

ppm

0.03

1 000

Samarium

Sm

ppm

0.03

1 000

Terbium

Tb

ppm

0.01

1 000

Thulium

Tm

ppm

0.01

1 000

Ytterbium

Yb

ppm

0.03

1 000

·      Laboratory inserted standards, blanks and duplicates were analysed per industry standard practice.  There was no evidence of bias from these results.

Verification of sampling and assaying

The verification of significant intersections by either independent or alternative company personnel.

The use of twinned holes.

Documentation of primary data, data entry procedures, data verification, data storage (physical and electronic) protocols.

Discuss any adjustment to assay data.

·      Two of the drillholes have been twinned, at Tors Tank where TT_005DD was drilled next to TT_003RC.

·      Conversion of elemental analysis (REE parts per million) to stoichiometric oxide (REO parts per million) was undertaken by ROM geological staff using the below element to stoichiometric oxide conversion factors (https://www.jcu.edu.au/news/releases/2020/march/rare-earth-metals-an-untapped-resource)

 

Table C1-1:  Element -Conversion Factor -Oxide Form

 

 

 

Ce

1.2284

CeO2

Dy

1.1477

Dy2O3

Er

1.1435

Er2O3

Eu

1.1579

Eu2O3

Gd

1.1526

Gd2O3

Ho

1.1455

Ho2O3

La

1.1728

La2O3

Lu

1.1371

Lu2O3

Nd

1.1664

Nd2O3

Pr

1.2083

Pr6O11

Sm

1.1596

Sm2O3

Tb

1.1762

Tb4O7

Tm

1.1421

Tm2O3

Y

1.2699

Y2O3

Yb

1.1387

Yb2O3

 

 

 

Rare earth oxide is the industry accepted form for reporting rare earths. The following calculations are used for compiling REO into their reporting and evaluation groups:

 

TREO (Total Rare Earth Oxide) = La2O3 + CeO2 + Pr6O11 + Nd2O3 + Sm2O3 + Eu2O3 + Gd2O3 + Tb4O7 + Dy2O3 + Ho2O3 + Er2O3 + Tm2O3 + Yb2O3 + Y2O3 + Lu2O3.

TREO-Ce = TREO - CeO2

LREO (Light Rare Earth Oxide) = La2O3 + CeO2 + Pr6O11 + Nd2O3 + Sm2O3 

HREO (Heavy Rare Earth Oxide) = Eu2O3 + Gd2O3 + Tb4O7 + Dy2O3 + Ho2O3 + Er2O3 + Tm2O3 + Yb2O3 + Y2O3 + Lu2O3

CREO (Critical Rare Earth Oxide) = Nd2O3 + Eu2O3 + Tb4O7 + Dy2O3 + Y2O3

MREO (Magnetic Rare Earth Oxide) = Pr6O11 + Nd2O3 + Sm2O3 + Gd2O3 + Tb4O7 + Dy2O3.

Total Rare Earth Oxides (TREO):

To calculate TREO an oxide conversion "factor" is applied to each rare-earth element assay.  The "factor" equates an elemental assay to an oxide concentration for each element. Below is an example of the factor calculation for Lanthanum (La):

Relative Atomic Mass (La) = 138.9055

Relative Atomic Mass (O) = 15.9994

Oxide Formula = La2O3

Oxide Conversion Factor = 1/ ((2x 138.9055)/(2x 138.9055 + 3x 15.9994)) Oxide Conversion Factor = 1.173 (3dp)

None of the historical data has been adjusted.

Location of data points

Accuracy and quality of surveys used to locate drill holes (collar and down-hole surveys), trenches, mine workings and other locations used in Mineral Resource estimation.

Specification of the grid system used.

Quality and adequacy of topographic control.

In general, locational accuracy does vary, depending upon whether the historical surface and drillhole samples were digitised off plans or had their coordinated tabulated.  Many samples were originally reported to AGD66 or AMG84 and have been converted to MGA94 (Zone 54)

The holes are currently surveyed with handheld GPS, awaiting more accurate DGPS survey.  It is thus estimated that locational accuracy therefore varies between 2-4m until the more accurate surveying is completed.  This assessment was confirmed once the holes were surveyed by DGPS from GMC Surveying.

The quality of topographic control (GSNSW 1 sec DEM) is deemed adequate for the purposes of the exploration drilling program.

Data spacing and distribution

Data spacing for reporting of Exploration Results.

Whether the data spacing and distribution is sufficient to establish the degree of geological and grade continuity appropriate for the Mineral Resource and Ore Reserve estimation procedure(s) and classifications applied.

Whether sample compositing has been applied.

The average sample spacing from the current drilling program across the tenure varies per prospect, and sample type, as listed in Table C1-2, below:

Table C1-2:  EL 8434 Drillhole Spacing

Prospect

Drillholes Completed

RMS Drillhole Spacing (m)

The Sisters

Not yet


Iron Blow

Not Yet


Tors Tank

4

127

Fence Gossan

4

208

Ziggy's Hill

n/a

n/a

Reefs Tank

4

221

The Datamine software allows creation of fixed length samples from the original database given a set of stringent rules.

Sample location is shown in Figure C1.

Figure C1: Location of Stage 1 Fence Gossan Surface Samples

Orientation of data in relation to geological structure

Whether the orientation of sampling achieves unbiased sampling of possible structures and the extent to which this is known, considering the deposit type.

If the relationship between the drilling orientation and the orientation of key mineralised structures is considered to have introduced a sampling bias, this should be assessed and reported if material.

Historical drill holes at the BHAE are typically drilled vertically for auger and RAB types (drilled along section lines) and angled at -55˚ or -60˚ to the horizontal and drilled perpendicular to the mineralised trend for RC and DDH.

Drilling orientations are adjusted along strike to accommodate folded geological sequences.  All Fence Gossan holes were designed to drill toward grid south at an inclination of 60 degrees from horizontal.

The drilling orientation is not considered to have introduced a sampling bias on assessment of the current geological interpretation.

Geological mapping by various companies has reinforced that the strata dips variously between 5 and 65 degrees.

Sample security

The measures taken to ensure sample security.

Sample security procedures are considered 'industry standard' for the current period.

Samples obtained during drilling completed between 4/10/22 to the 10/10/22 were transported by exploration employees or an independent courier directly from Broken Hill to ALS Laboratory, Adelaide.

The Company considers that risks associated with sample security are limited given the nature of the targeted mineralisation.

Audits or reviews

The results of any audits or reviews of sampling techniques and data.

No external audits or reviews have yet been undertaken.

 


SECTION 2: REPORTING OF EXPLORATION RESULTS

Criteria

JORC Code explanation

Commentary

Mineral tenement and land tenure status

Type, reference name/number, location and ownership including agreements or material issues with third parties such as joint ventures, partnerships, overriding royalties, native title interests, historical sites, wilderness or national park and environmental settings.

The security of the tenure held at the time of reporting along with any known impediments to obtaining a licence to operate in the area.

EL 8434 is located about 28km east of Broken Hill whilst EL 8435 is 16km east of Broken Hill.  Both tenures are approximately 900km northwest of Sydney in far western New South Wales (Figures C2-1 and C2-2 in Appendix A &B, above). 

EL 8434 and EL 8435 were both granted on the 2nd of June 2016 to Squadron Resources for a term of five (5) years for Group One Minerals.  On the 25th of May 2020, Squadron Resources changed its name to Wyloo Metals Pty Ltd (Wyloo).  In December 2020 the tenure was transferred from Wyloo Metals to Broken Hill Alliance Pty Ltd a 100% subsidiary company of Castillo Copper Limited.  Both tenures were renewed on the 12th of August 2021 for a further six (6) years and are due to expire on the 2nd of June 2027.

EL 8434 lies across two (2) 1:100,000 geology map sheets Redan 7233 and Taltingan 7234, and two (2) 1:250,000 geology map sheets, SI54-3 Menindee, and SH54-15 Broken Hill in the county of Yancowinna.  EL 8434 consists of one hundred and eighty-six (186) units) in the Adelaide and Broken Hill 1:1,000,000 Blocks covering an area of approximately 580km2.

EL 8435 is located on the 1:100,000 geology map sheet Taltingan 7234, and the 1:250,000 geology map sheet SH/54-15 Broken Hill in the county of Yancowinna.  EL 8435 consists of twenty-two (22) units (Table 1) in the Broken Hill 1:1,000,000 Blocks covering an area of approximately 68km2.

Access to the tenures from Broken Hill is via the sealed Barrier Highway.  This road runs north-east to south-west through the northern portion of the EL 8434, passes the southern tip of EL 8435 eastern section and through the middle of the western section of EL 8435.  Access is also available via the Menindee Road which runs north-west to south-east through the southern section of the EL 8434.  The Orange to Broken Hill Rail line also dissects EL 8435 western section the middle and then travels north-west to south-east slicing through the eastern arm of EL 8434 (Figure C2-1).

Figure C2-1:  EL 8434 and EL 8435 General Location Map

Exploration done by other parties

Acknowledgment and appraisal of exploration by other parties.

Explorers who were actively involved over longer historical periods in various parts of EL8434 were: - North Broken Hill Ltd, CRAE Exploration, Major Mining Ltd and Broken Hill Metals NL, Pasminco Exploration Ltd, Normandy Exploration Ltd, PlatSearch NL/Inco Ltd/ EGC Pty Ltd JV and the Western Plains Gold Ltd/PlatSearch/EGC Pty Ltd JV.

A comprehensive summary of work by previous explorers was presented in Leyh (2009). However, more recently, follow-up field reconnaissance of areas of geological interest, including most of the prospective zones was carried out by EGC Pty Ltd over the various licenses. This work, in conjunction with a detailed interpretation of aeromagnetic, gravity plus RAB / RC drill hole logging originally led to the identification of at least sixteen higher priority prospect areas. All these prospects were summarized in considerable detail in Leyh (2008).  Future work programs were then also proposed for each area.  Since then, further compilation work plus detailed geological reconnaissance mapping and sampling of gossans and lode rocks has been carried out.

A total of 22 prospects were then recognised on the exploration licence with at least 12 occurring in and around the tenure.

With less than 45% outcropping Proterozoic terrain within the licence, this makes it very difficult to explore and is in the main very effectively screened from the easy application of more conventional exploration methodologies due to a predominance of extensive Cainozoic cover sequences.  These include recent to young Quaternary soils, sands, clays and older more resistant, only partially dissected, Tertiary duricrust regolith covered areas.  Depth of cover ranges from a few metres in the north to over 60 metres in some areas on the southern and central license.

Exploration by EGC Pty Ltd carried out in the field in the first instance has therefore been heavily reliant upon time consuming systematic geological reconnaissance mapping and relatable geochemical sampling.  These involve a slow systematic search over low outcropping areas, poorly exposed subcrops and float areas as well as the progressive development of effective regolith mapping and sampling tools.  This work has been combined with a vast amount of intermittently acquired past exploration data.  The recent data compilation includes an insufficiently detailed NSWGS regional mapping scale given the problems involved, plus some regionally extensive, highly variable, low-level stream and soil BLEG geochemical data sets over much of the area. 

There are also a few useful local detailed mapping grids at the higher priority prospects, and many more numerous widespread regional augers, RAB, and percussion grid drilling data sets. Geophysical data sets including ground magnetics, IP and EM over some prospect areas have also been integrated into the exploration models.  These are located mainly in former areas of moderate interest and most of the electrical survey methods to date in this type of terrain continue to be of limited application due to the high degree of weathering and the often prevailing and complex regolith cover constraints.

Between 2007 and 2014 Eaglehawk Geological Consulting has carried out detailed research, plus compilation and interpretation of a very large volume of historic exploration data sourced from numerous previous explorers and dating back to the early 1970's. Most of this data is in non-digital scanned form. Many hard copy exploration reports (see references) plus several hundred plans have been acquired from various sources, hard copy printed as well as downloaded as scans from the Geological Survey of NSW DIGS system. They also conducted field mapping, costean mapping and sampling, and rock chip sampling and analysis.

Work Carried out by Squadron Resources and Whyloo Metals 2016-2020

Research during Year 1 by Squadron Resources revealed that the PGE-rich, sulphide-bearing ultramafic rocks in the Broken Hill region have a demonstrably alkaline affinity.  This indicates a poor prospectivity for economic accumulations of sulphide on an empirical basis (e.g., in comparison to all known economic magmatic nickel sulphide deposits, which have a dominantly tholeiitic affinity).  Squadron instead directed efforts toward detecting new Broken Hill-Type (BHT) deposits that are synchronous with basin formation.  Supporting this modified exploration rationale are the EL's stratigraphic position, proximity to the Broken Hill line of lode, abundant mapped alteration (e.g., gahnite and/or garnet bearing exhalative units) and known occurrences such as the "Sisters" and "Iron Blow" prospects.

The area overlies a potential magmatic Ni-Cu-PGE source region of metasomatised sub-continental lithospheric mantle (SCLM) identified from a regional targeting geophysical data base.  The exploration model at the time proposed involved remobilization of Ni-Cu-PGE in SCLM and incorporation into low degree mafic-ultramafic partial melts during a post-Paleoproterozoic plume event and emplacement higher in the crust as chonoliths/small intrusives - Voisey's Bay type model.  Programs were devised to use geophysics and geological mapping to locate secondary structures likely to control and localise emplacement of Ni-Cu-PGE bearing chonoliths. Since EL8434 was granted, the following has been completed:

•           Airborne EM survey.

•           Soil and chip sampling.

•           Data compilation.

•           Geological and logistical reconnaissance.

•           Community consultations; and

•           Execution of land access agreements.

Airborne EM Survey

Geotech Airborne Limited was engaged to conduct an airborne EM survey using their proprietary VTEM system in 2017.  A total of 648.92-line kilometres were flown on a nominal 200m line spacing over a portion of the project area. Several areas were infilled to 100m line spacing.

The VTEM data was interpreted by Southern Geoscience Consultants Pty Ltd, who identified a series of anomalies, which were classified as high or low priority based on anomaly strength (i.e., does the anomaly persist into the latest channels).  Additionally, a cluster of VTEM anomalies at the "Sisters" prospect have been classified separate due to strong IP effects observed in the data.  Geotech Airborne have provided an IP corrected data and interpretation of the data has since been undertaken.

Soil and Chip sampling

The VTEM anomalies were followed up by a reconnaissance soil sampling programme. Spatially clustered VTEM anomalies were grouped, and follow-up soil lines were designed.  Two (2) VTEM anomalies were found to be related to culture and consequently no soils were collected.  Two (2) other anomalies were sampled which were located above thick alluvium of Stephens Creek and were therefore not sampled.  A line of soil samples was collected over a relatively undisturbed section at Iron Blow workings and the Sisters Prospect.

One hundred and sixty-six (166) soil samples were collected at a nominal 20cm depth using a 2mm aluminum sieve.  Two (2) rock chips were also collected during this program.  The samples were collected at either 20m or 40m spacing over selected VTEM anomalies.  The samples were pulverised and analysed by portal XRF at ALS laboratories in Perth.

Each site was annotated with a "Regolith Regime" such that samples from a depositional environment could be distinguished from those on exposed Proterozoic bedrock, which were classified as an erosional environment.  The Regolith Regime groups were used for statistical analysis and levelling of the results.  The levelled data reveals strong relative anomalies in zinc at VTEM anomaly clusters 10, 12 and 14 plus strong anomalous copper at VTEM 17.

Geology

Deposit type, geological setting, and style of mineralisation.

As the strata is tightly folded, the intersected cobalt-rich layers are overstated in terms of apparent thickness, however the modelling software calculates a true, vertical thickness.  Cobalt mineralisation is commonly associated with shears, faults, amphibolites, and a quartz-magnetite rock within the shears, or on or adjacent to the boundaries of the Himalaya Formation. In general, most of the cobalt and rare earth element - rich layers have a north-northwest to north strike.

REE enrichment generally occurs as a 5 to 10-metre-thick zone between the completely weathered layer and strongly weathered layer and it is targeted for commercial mining (Figure D2-2).  Compared to other REE deposits, regolith-hosted rare earth element deposits are substantially low-moderate grade (containing 0.05-0.3 wt.% extractable REEs).  Nevertheless, due to its easy extraction method, low processing costs and large abundance, the orebodies are generally economic to be extracted (Duuring, (2020); Kanazawa and Kamitani (2006); and Murakami, H.; Ishihara (2008)).

Figure C2-2: Weathering Profile over REE - Rich Granite

A picture containing chart Description automatically generated

https://en.wikipedia.org/wiki/Regolith-hosted_rare_earth_element_deposits

Weathering profile of regolith hosted REE deposits shown above, the legend is: (A) Humic layer. (B) Completely weathered layer. (C) Strongly weathered layer. (D) Weathering front. (E) Unweathered rock.

Most of the REE found in cerium monazite (Ce (PO4)) which always contains major to minor amounts of other REE (Nd, La, Pr, Sm etc) replacing Ce.  Also, the mineral often contains trace amounts of U and Th (coupled with Ca).  This will be collaborated with XRD and or SEM analysis. 

Drill hole Information

A summary of all information material to the understanding of the exploration results including a tabulation of the following information for all Material drill holes:

easting and northing of the drill hole collar

elevation or RL (Reduced Level - elevation above sea level in metres) of the drill hole collar

dip and azimuth of the hole

down hole length and interception depth

hole length.

If the exclusion of this information is justified on the basis that the information is not Material and this exclusion does not detract from the understanding of the report, the Competent Person should clearly explain why this is the case.

Header information about all drillholes and surface samples completed at Tors Tank and Fence Gossan have been tabulated in this release in Appendix B.

Data aggregation methods

In reporting Exploration Results, weighting averaging techniques, maximum and/or minimum grade truncations (e.g., cutting of high grades) and cut-off grades are usually Material and should be stated.

Where aggregate intercepts incorporate short lengths of high-grade results and longer lengths of low-grade results, the procedure used for such aggregation should be stated and some typical examples of such aggregations should be shown in detail.

The assumptions used for any reporting of metal equivalent values should be clearly stated.

No metal equivalents have been reported.  Rare earth element results have been converted to rare earth oxides as per standard industry practice (Castillo Copper 2022f).

No compositing of assay results has taken place, but rather menu options within the Datamine GDB module have been used to create fixed length 1m assay intervals from the original sampling lengths.

The rules follow very similarly to those used by the Leapfrog Geo software in creating fixed length samples.

Relationship between mineralisation widths and intercept lengths

These relationships are particularly important in the reporting of Exploration Results.

If the geometry of the mineralisation with respect to the drill hole angle is known, its nature should be reported.

If it is not known and only the down hole lengths are reported, there should be a clear statement to this effect (e.g., 'down hole length, true width not known').

A database of all the historical borehole sampling has been compiled and validated. It is uncertain if there is a strong relationship between the surface sample anomalies to any subsurface anomalous intersections due to the possible masking by variable Quaternary and Tertiary overburden that varies in depth from 0-15m.  The mineralisation appears to be secondary enrichment in the regolith clays and extremely weathered material derived from quartzo-feldspathic pegmatites.  

Diagrams

Appropriate maps and sections (with scales) and tabulations of intercepts should be included for any significant discovery being reported These should include, but not be limited to a plan view of drill hole collar locations and appropriate sectional views.

Current surface anomalies are shown on maps released on the ASX (Castillo Copper 2022d, 2022e, 2022f and 2022g).  All historical surface sampling has had their coordinates converted to MGA94, Zone 54.

Balanced reporting

Where comprehensive reporting of all Exploration Results is not practicable, representative reporting of both low and high grades and/or widths should be practiced to avoid misleading reporting of Exploration Results.

All recent laboratory analytical results have been recently reported (see Castillo Copper 2022a, b, c, d, e, f, and g) for assay results.

Regarding the surface and sampling, no results other than duplicates, blanks or reference standard assays have been omitted.

Other substantive exploration data

Other exploration data, if meaningful and material, should be reported including (but not limited to): geological observations; geophysical survey results; geochemical survey results; bulk samples - size and method of treatment; metallurgical test results; bulk density, groundwater, geotechnical and rock characteristics; potential deleterious or contaminating substances.

Historical explorers have also conducted airborne and ground gravity, magnetic, EM, and IP resistivity surveys over parts of the tenure area but this is yet to be fully georeferenced (especially the ground IP surveys). Squadron Resources conducted an airborne EM survey in 2017 that covers Iron Blow and The Sisters, but not the southern cobalt and REE prospects.

Further work

The nature and scale of planned further work (e.g., tests for lateral extensions or depth extensions or large-scale step-out drilling).

Diagrams clearly highlighting the areas of possible extensions, including the main geological interpretations and future drilling areas, provided this information is not commercially sensitive.

It is recommended that:

·      Complete rehabilitation of the 2022 BHAE drilling campaign that comprised mostly RC drilling.  An application supporting an  ESF2 lodgment is yet to be approved by the NSW Resource Regulator

·      The remaining non-sampled zones within the Core Library drillholes, BH1, BH2, and DD90-IB3 in the north of the tenure group be relogged and sampled.  DD90-IB3 had 21-87m retested recently and is a good candidate for hyperspectral logging.

·      A program of field mapping and ground magnetic, IP or radiometric surveys be planned and executed at Fence Gossan.  Mapping of pegmatite outcrops is a high priority.

·      Generate an Exploration Target for Fence Gossan to the standard of Clause 17 of the 2012 JORC Code.

·      Depending upon the results of the proposed geophysical surveys and Exploration Target noted above, the next drilling program will specifically target the air coring technique over the known cobalt and REE mineralisation downdip to at least 30m depth at all three prospects.  That proposed drilling program is also designed to increase the resource confidence of the REE to Inferred Resources to the standard of the 2012 JORC Code.

 


REFERENCES

Biggs, M. S., 2021a, Broken Hill Alliance, NSW Tenure Package Background Geological Information, unpublished report to BH Alliance Pty Ltd, Sep 21, 30pp.

Biggs, M. S., 2021b, EL 8434 and EL 8435, Brief Review of Surface Sample Anomalies Lithium, Rare Earth Elements and Cobalt, unpublished report to BH Alliance Pty Ltd, Nov 21, 18pp.

Biggs, M.S., 2022a, BHA Cobalt Modelling and Mineral Resource Estimate Update, unpublished memo for Castillo Copper by ROM Resources.

Biggs, M.S., 2022b, Broken Hill BHA Tenures Update, Castillo Copper, unpublished memo prepared by ROM Resources, Mar 22, 5pp.

Biggs M.S., 2022c, Geological Briefing Paper, Iron Blow Prospect, East Zone, BHA Project (BHAE), Broken Hill, NSW, ROM Resources, prepared for Castillo Copper Limited, August 2022

Burkett R.D., 1975, Progress Report on Exploration Licenses 780, 781, 782 and 783, Broken Hill Area, NSW for the six months to 23rd November 1975, North Broken Hill Limited for the NSW Geological Survey, (GS1975-328)

Castillo Copper Limited, 2020, ASX Release Acquisition enhances BHT (zinc-silver-lead) and IOCG (gold-copper) prospectivity at Broken Hill, 1st October 2020.

Castillo Copper Limited, 2022a, ASX Release Battery metal drill-hole assays unlock BHA East Zone potential / lithium update, 5th January 2022.

Castillo Copper Limited, 2022b, ASX Release Strategic focus to develop significant cobalt mineralisation potential at BHA Project, 9th February 2022.

Castillo Copper Limited, 2022c, ASX Release High grade platinum confirmed at BHA Project, 9th March 2022.

Castillo Copper Limited, 2022d ASX Release Diamond core tests demonstrate high-grade cobalt-zinc potential at Broken Hill, 21 March 2022

Castillo Copper Limited, 2022e ASX Release, Drilling hits targeted cobalt zones & wide pegmatite intercepts at Broken Hill 12 October 2022

Castillo Copper Limited, 2022f ASX Release, Drilling hits more wide pegmatite intercepts at Broken Hill, 24 October 2022

Castillo Copper Limited, 2022g ASX Release, Completed auger sampling campaign targets 6.5km2 REE mineralisation zone, 23 December 2022

Duuring, P 2020, Rare-element pegmatites: a mineral systems analysis: Geological Survey of Western Australia, Record 2020/7, 6p.

Kanazawa, Y.; Kamitani, M., 2006, "Rare earth minerals and resources in the world". Journal of Alloys and Compounds. 408: 1339-1343. doi:10.1016/j.jallcom.2005.04.033

Lees, T.C., 1978, Progress Report on Farmcote Exploration Licenses 780 and 782, Farmcote Area, Broken Hill, NSW for the six months to 23RD November 1978, North Broken Hill Limited for the NSW Geological Survey, (GS1978-043)

Leyh, W.R., 1976, Progress Report on Exploration Licence, No. 846 Iron Blow -Yellowstone Area, Broken Hill, New South Wales for the six months period ended 29th June 1976, North Broken Hill Limited, Report GS1976-198, Jul 76, 88pp.

Leyh, W.R., 1977a, Progress Report on Exploration Licence, No. 846 Iron Blow -Yellowstone Area, Broken Hill, New South Wales for the six months period ended 29th December 1976, North Broken Hill Limited, Report GS1976-198, Feb 1977, 24pp.

Leyh W.R., 1977b, Progress Report on Farmcote Exploration Licenses 780 and 782, Farmcote Area, Broken Hill, NSW for the three months to 5th March 1977, North Broken Hill Limited for the NSW Geological Survey, (GS1977-078)

Leyh W.R., 1977c, Progress Report on Farmcote Exploration Licenses 780 and 782, Farmcote Area, Broken Hill, NSW for the three months to 23rd May 1977, North Broken Hill Limited for the NSW Geological Survey, (GS1977-078)

Leyh W.R., 1978, Progress Report on Farmcote Exploration Licenses 780 and 782, Farmcote Area, Broken Hill, NSW for the three months to 27 October 1978, North Broken Hill Limited for the NSW Geological Survey, (GS1977-078)

Leyh W.R., 1978 Progress Report on Exploration Licenses 1099 and 1100 for the six months to 27 October 1978, North Broken Hill Limited for the NSW Geological Survey, (GS1978-407).

Leyh, W.R., 1990, Exploration Report for the Third Six Monthly Period ended 12th June 1990 for EL 3238 (K Tank), Broken Hill District, New South Wales for the six months period, Pasminco Limited, Report GS1989-226, Jun 90, 22pp.

Leyh, W.R., and Lees T.C., 1977, Progress Report on Exploration Licence, No. 846 Iron Blow -Yellowstone Area, Broken Hill, New South Wales for the six months period ended 29th June 1977, North Broken Hill Limited, Report GS1976-198, Jul 77, 35pp.

Leyh, W.R., and Larson P.D., 1981, Final Report for the Third Six Monthly Period ended 12th June 1990 for EL 3238 (K Tank), Broken Hill District, New South Wales for the six months period, Pasminco Limited, Report GS1989-226, Jun 90, 22pp.

McConachie, G.W., 1997, EL 4792 Redan, Annual Report for the period ending 19/2/1997, Normandy Exploration Limited, unpublished report to the GSNSW, RIN 00002672

Main, J.V., and Tucker D.F., 1981, Exploration Report for Six Month Period 8th November 1980 to 7th May 1981, EL 1106 Rockwell, Broken Hill, NSW, CRA Exploration Pty Ltd, GS1980-080, Jul 1981, 40pp

Mohoney, M., 2018, BHA Broken Hill Project Position Paper, Squadron Resources Pty Ltd., Unpublished report, Mar2018, 8pp.

Mortimer R., 2017, Re-interpretation of VTEM Profiles Broken Hill Area, unpublished report by Southern Geoscience Consultants for Squadron Resources Pty Ltd, Oct 17.

https://en.wikipedia.org/wiki/Regolith-hosted_rare_earth_element_deposits

Murakami, H.; Ishihara, S., 2008, REE mineralization of weathered crust and clay sediment on granitic rocks in the Sanyo Belt, SW Japan and the Southern Jiangxi Province, China". Resource Geology. 58 (4): 373-401. doi:10.1111/j.1751-3928.2008.00071.x.

Segnit, E.R. (1946) Barium-feldspars from Broken Hill, New South Wales. Mineralogical Magazine, 27, 166-174.

Squadron Resources Pty Ltd, 2018, Broken Hill Project Status, August 2018, unpublished confidential presentation by Squadron Resources,

Timms, P.D., and Groves A.J., 2003, Exploration Licence 4846, The Sisters, Annual Report to 29th May 2003, Endeavour Minerals Pty Ltd., RIN

Willis, I.L., Brown, R.E., Stroud, W.J., Stevens, B.P.J., 1983, The Early Proterozoic Willyama Supergroup: stratigraphic subdivision and interpretation of high to low-grade metamorphic rocks in the Broken Hill Block, New South Wales., Geological Society of Australia Journal, 30(2), p195-2

 

 

 

 

 

 

 

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