greenx metals limited
NEWS RELEASE 9 NOVEMBER 2022
HIGHLY ENCOURAGING RESULTS FROM INITIAL ARC SITE VISIT
· | High-grade copper sulphides verified at the ARC Discovery Zone prospect hosted within a Black Earth fault zone |
· | An insitu peak sample grading 53.8% copper and 1,074 g/t silver, located along strike from historically reported float sample also grading 53.8% Cu with 2,480 g/t Ag |
· | Further along strike to the west, a well exposed zone is visually estimated to be around 5m wide, from which a pXRF analysis yielded a median of 4.47% Cu and 91 g/t Ag, verifying a historical report of 4.42% Cu and 187.5 g/t Ag from a 3m long trench |
· | Mineralisation was also identified in sandstones flanking the Black Earth zone, with pervasive veins and veinlets of chalcocite being observed |
· | High grade 'fissure' containing visible native copper located at Neergaard Dal |
· | Site visit provided confirmation of the opportunity to establish a logistical base in Greenland which will expedite future exploration programs |
GreenX Metals Ltd (GreenX or the Company) and its joint-venture (JV) partner Greenfields Exploration Ltd (Greenfields) are pleased to announce the results from the first site visit to the Arctic Rift Copper Project (ARC) in Greenland. The results of this work program have demonstrated the high-grade nature of the known copper sulphide mineralization, and wider copper mineralization in fault hosted Black Earth zones and adjacent sandstone units. The exact position of a native copper fissure at the Neergaard Dal prospect was also identified. This new information is key to future targeting of stratabound copper of both types.
The field team completed a site visit to the Discovery Zone and Neergaard Dal prospects in the northern half of ARC.
A sample at the Discovery Zone prospect yielded a peak reading of 53.8% Cu with 1,074 g/t Ag; and an average reading of 39.3% Cu and 1,065 g/t Ag (refer to Appendix 1). Other samples at the Discovery Zone yielded 12.09% Cu and 373 g/t Ag; with a median result of some being 5.82% Cu and 448 g/t Ag.
One of the objectives of the site visit was to verify the Discovery Zone, given the extremely high grades reported historically. The location of the high-grade material was apparent from over 150m altitude and on the ground. Finding the native copper mineralisation at Neergaard Dal was similarly easy. Historically, a copper fissure was noted but this was recorded prior to GPS and so the exact location was unknown. A well-mineralised fissure was quickly identified, which bodes well for finding additional fissures in this area and further afield. Portable XRF (pXRF) readings were taken of the collected samples. These results are summarized below and presented in Appendix 1.
Dr Bell, Project Leader said: "The historically reported high grade copper sulphides and fissure copper were located with relative ease during the site visit. Both were immediately apparent on the first pass flying over the sites. The ease with which the historically reported mineralisation was identified in the field bodes well for in terms of forward work programs to locate and map stratabound mineralisation that may have bulk tonnage potential."
DISCOVERY ZONE
Samples were collected from the Discovery Zone fault-hosted 'Black Earth' and sandstone-hosted mineralisation. Historical sampling from this area demonstrates 4.5m true width of 2.15% Cu, 35.5 g/t Ag (see the Company's news release dated 6 October, 2021). The dominant copper mineral is chalcocite, which occurs as pervasive thin veins that sometimes produce visually obvious green oxides like malachite. The primary trend of the mineralisation appears to be bounded by a sub-vertical sandstone fault that produces a prominent ~2m ledge (5). As the mineralised fault is softer than the sandstone, it has a negative relief and is superficially obscured in places.
The Black Earth material comprises a variety of different rock types hosted by fine-grained material. There appear to be at least four subtly different sandstones and mudstones, as well as fragments of very dense, almost complete chalcocite. This dense material is almost the same as that is historically reported to grade 53.8% copper ('Cu') and 2,480 silver ('Ag'). A handheld XRF unit was used to conduct multiple scans of sample A1199a, which also yielded a peak reading of 53.8% Cu with 1,074 g/t Ag; and average reading of 39.3% Cu and 1,065 g/t Ag (6). This high-grade sample was recovered from 35m along strike to the west of where a similar grading float sample was historically collected. The Company cautions that pXRF readings are indicative and not absolute. It is possible that surface oxidation and contamination produced lower readings than may be recorded from the central mass of A1199a. The shape of sample A1199a is suggestive of something tabular, like that of the historical sample with extreme grades. This tabular shape could result from a vein, like the fine-grained chalcocite veinlets seen throughout the area or a layer within the sedimentary horizon. Notably, the other Black Earth material hosting this high-grade material is also mineralised, as is the surrounding sandstone. The median XRF reading of the six fragments (A1199a to A1199f) is 12.09% Cu and 373 g/t Ag; and the median of all the 49 Black Earth readings (including A1197a-d, A1198a-d) is 5.48% Cu and 89 g/t Ag. The samples 1197 and 1198 are of interest as they are from an area where the Black Earth is well exposed, and has an apparent width around 5 m.
In addition to an analysis of the largest clasts above from the Black Earth samples that were washed cleaned, XRF readings were taken directly of the material inside the sample bag. Visually, this material is dominated by loose, individual quartz grains, and grey clay (7) and was expected to give very low copper and silver readings. However, seven XRF readings of sample A1199a indicate that the fine-grained material has a median grade of 5.82% Cu and 448 g/t Ag. As this fine-grained material coats all the larger grains, the Company interprets that there is chalcocite within the clays. Similarly, the median XRF readings of all the fines (not just clay-rich material) is 4.86% Cu, 124.5 g/t Ag. This is important as it means that significant mineralisation is present in all the apparent size fractions, which may reduce any 'nugget effect' of the clasts in the Black Earth. The Company will undertake further analysis to assess the distribution of copper and silver throughout the various size fractions of the Black Earth material.
The sandstone flanking the fault that hosts the Black Earth is also mineralised. Samples from this material show veins and veinlets of chalcocite that lead to prominent malachite stains. In some instances, the veins are millimetres thick (8), but often they are thinner and more pervasive throughout zones in the rock mass (9). This extends the search space for copper mineralisation to the outside of the immediate area of the fault zone.
NEERGAARD DAL
The fissure investigated by the Company at Neergaard Dal is one of several fissures reported in the area. The fissure is estimated to be around 20m thick and strikes in a north-south orientation. The fissure is well mineralised in the western half, with native copper and cuprite. The investigated area also exposes a portion of what may be the 'Red Marker' (historically called the Red Flow). A sketch from the year 1979 shows that a fissure extends vertically from a stratigraphic position above the Red Marker, topographically higher than that observed by the Company. At surface, this gives the fissure more than 200m vertical extent and a strike of more than 600m. By comparing the position of the Red Marker, the Company also identifies the stratabound "copper-containing gas cavities" is exposed in the southern slope of the same valley. Such stratabound 'amygdaloidal' mineralisation contained significant tonnages of copper in other regions such as Keweenaw, USA. This will be verified as a priority in future field programs.
Samples collected from the newly located fissure at Neergaard Dal weighed up to ~ 10kg. The samples were collected from scree that derived from the fissure. The western margin of the scree contains extensive, largely disseminated copper mineralisation. The visually dominant copper mineral is cuprite which coats the native copper. The samples collected by the Company contain pervasive fine-grained, sub-millimetre cuprite, and more occasional millimetre-scale grains with unaltered native copper at their core. In turn, the cuprite is associated with haloes of malachite, making the mineralisation visually distinctive in the field. The pXRF analysis of the most westerly, and mineralised samples (A1196b, c) resulted in median readings of 4.78% Cu and 5.0 g/t Ag; and 1.44% Cu and 7.0 g/t Ag.
LOGISTICS
The main thrust of the 2022 site visit was to establish a logistical base in Greenland. The Company successfully established depots, and field trialed the Sherp vehicles and advanced satellite communications systems. However, the expansion of war in Ukraine directly impacted and exacerbated the worst global logistical framework in 75 years and this was further compounded by the densest sea-ice conditions in thirty years. Accordingly, much of this field season's planned geological work has been deferred until the next field season. However, having the explorations assets already in Greenland will benefit and expedite the next field program at ARC.
ABOUT THE ARCTIC RIFT COPPER PROJECT
ARC is an exploration joint venture between GreenX and Greenfields. GreenX can earn up to 80% by spending a total of A$10 M by October 2026. The ARC Project is targeting large-scale copper in multiple settings across a 5,774 km2 Special Exploration Licence in eastern North Greenland. It sits within the newly identified, and underexplored Kiffaanngissuseq metallogenic province. This province is considered analogous to the Keweenaw Peninsula of Michigan, USA, which contained a pre-mining endowment of +7 Mt of copper in sulphides and 8.9 Mt of native copper. Like Keweenaw, ARC contains, high-grade copper sulphides, 'fissure' native copper, and native copper contained in what were formerly gas bubbles and layers between lava flows.
-ENDS-
Competent Persons Statement
Information in this announcement that relates to Exploration Results is based on information compiled by Dr Jonathan Bell, a Competent Person who is a member of the Australian Institute of Geoscientists (AIG). Dr Bell is the Managing Director of Greenfields Exploration Limited and holds an indirect interest in performance rights in GreenX. Dr Bell has sufficient experience that is relevant to the style of mineralisation and type of deposit under consideration and to the activity being undertaken, to qualify as a Competent Person as defined in the 2012 Edition of the 'Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves'. Dr Bell consents to the inclusion in this announcement of the matters based on his information in the form and context in which it appears.
To view this announcement in full, including all illustrations, figures and notes, please refer to www.greenxmetals.com.
Appendix 1: Portable XRF RESULTS
Sample | Sub | Reading No | Location | Lat_Y WGS84 | Long''_X WGS84 | Cu % | Ag ppm | Pb ppm | Pd ppm | Sn ppm | As ppm | Hg ppm | Cd ppm | Fe % | S ppm | K % |
A1197 | d | 235 | Discovery Zone | 81.95527 | -26.20158 | 56.6 | 1371 | 110 | | 76 | 1621 | | | 3.0 | 85645 | 0.6 |
A1199 | b | 201 | Discovery Zone | 81.95516 | -26.20024 | 53.8 | 893 | 329 | | | 1429 | | | 4.0 | 70436 | 1.2 |
A1199 | a | 198 | Discovery Zone | 81.95516 | -26.20024 | 52.0 | 1769 | 176 | | 80 | 1174 | | | 3.6 | 77901 | 1.1 |
A1199 | d | 210 | Discovery Zone | 81.95516 | -26.20024 | 51.1 | 709 | 130 | | 41 | 390 | | | 5.6 | 75839 | 1.3 |
A1199 | b | 202 | Discovery Zone | 81.95516 | -26.20024 | 47.8 | 1074 | 324 | 15 | 73 | 1213 | | | 5.0 | 89759 | 1.2 |
A1199 | d | 212 | Discovery Zone | 81.95516 | -26.20024 | 42.6 | 1067 | 200 | 9 | 88 | 768 | | | 6.5 | 39741 | 2.6 |
A1215 | a | 158 | Discovery Zone | 81.95586 | -26.20112 | 39.5 | | | | 79 | 8 | | | 0.4 | 17247 | 0.2 |
A1199 | a | 200 | Discovery Zone | 81.95516 | -26.20024 | 39.4 | 878 | 138 | 8 | 109 | 564 | | | 4.0 | 64967 | 2.3 |
A1197 | c | 231 | Discovery Zone | 81.95527 | -26.20158 | 37.0 | 863 | 42 | 9 | 65 | 533 | | 10 | 2.8 | 69950 | 1.3 |
A1199 | d | 214 | Discovery Zone | 81.95516 | -26.20024 | 29.9 | 342 | 186 | 9 | 52 | 700 | 13 | | 4.9 | 37830 | 1.9 |
A1215 | a | 257 | Discovery Zone | 81.95586 | -26.20112 | 27.7 | 11 | | | 57 | 6 | 20 | | 0.4 | 54221 | 0.2 |
A1196 | a | 57 | Neergaard Dal | 81.78512 | -26.66043 | 27.7 | 17 | | | 42 | 17 | 11 | | 1.7 | 773 | 0.3 |
A1215 | a | 258 | Discovery Zone | 81.95586 | -26.20112 | 27.5 | | | | 39 | 10 | | | 0.3 | 57962 | 0.2 |
A1199 | a | 199 | Discovery Zone | 81.95516 | -26.20024 | 26.5 | 547 | 118 | 10 | 52 | 319 | | | 1.7 | 45657 | 1.9 |
A1215 | a | 256 | Discovery Zone | 81.95586 | -26.20112 | 26.5 | | | | 43 | 6 | | | 0.3 | 29648 | 0.3 |
A1196 | b | 70 | Neergaard Dal | 81.78512 | -26.66043 | 26.4 | 15 | | | 64 | 8 | 11 | | 2.1 | 2257 | 0.6 |
A1215 | a | 255 | Discovery Zone | 81.95586 | -26.20112 | 24.5 | | | | 27 | 4 | | | 0.5 | 35844 | 0.4 |
A1215 | a | 153 | Discovery Zone | 81.95586 | -26.20112 | 23.4 | 14 | | | 45 | 5 | | | 0.4 | 54563 | 0.2 |
A1215 | a | 254 | Discovery Zone | 81.95586 | -26.20112 | 22.3 | | | | 27 | 5 | | | 0.5 | 32314 | 0.3 |
A1215 | a | 152 | Discovery Zone | 81.95586 | -26.20112 | 22.2 | 18 | | | 39 | 4 | | | 0.4 | 58970 | 0.2 |
A1195 | b | 189 | Neergaard Dal | 81.78532 | -26.66077 | 20.4 | 10 | | | 58 | 14 | | | 1.3 | 507 | 0.3 |
A1196 | b | 72 | Neergaard Dal | 81.78512 | -26.66043 | 18.7 | 10 | | | 58 | 11 | | | 2.3 | 436 | 0.5 |
A1199 | b | 203 | Discovery Zone | 81.95516 | -26.20024 | 16.2 | 405 | 82 | 7 | 37 | 388 | | | 2.3 | 38175 | 2.5 |
A1196 | b | 65 | Neergaard Dal | 81.78512 | -26.66043 | 15.7 | 6 | | | 51 | | | | 2.0 | 655 | 0.1 |
A1196 | d | 76 | Neergaard Dal | 81.78512 | -26.66043 | 15.2 | | | | 49 | 29 | | | 2.3 | 95 | 0.1 |
A1215 | a | 157 | Discovery Zone | 81.95586 | -26.20112 | 15.1 | 8 | | | 31 | 6 | | | 0.5 | 26681 | 0.4 |
A1199 | f | 219 | Discovery Zone | 81.95516 | -26.20024 | 14.6 | 1364 | 208 | 5 | 38 | 747 | | | 8.0 | 29867 | 1.6 |
A1196 | a | 64 | Neergaard Dal | 81.78512 | -26.66043 | 14.3 | | | | 18 | | | | 1.6 | | 0.1 |
A1196 | bag fines | 286 | Neergaard Dal | 81.78512 | -26.66043 | 14.0 | 12 | | 3 | 26 | 11 | | | 2.2 | 184 | 0.1 |
A1199 | b | 204 | Discovery Zone | 81.95516 | -26.20024 | 13.9 | 262 | 71 | 5 | 19 | 412 | | | 2.1 | 36211 | 2.1 |
A1196 | c | 75 | Neergaard Dal | 81.78512 | -26.66043 | 13.5 | 9 | | | 43 | 44 | | | 2.2 | 765 | 0.2 |
A1196 | b | 69 | Neergaard Dal | 81.78512 | -26.66043 | 13.4 | | | | 64 | 12 | | | 2.9 | 886 | 0.4 |
A1198 | a | 137 | Discovery Zone | 81.95524 | -26.20146 | 13.3 | 323 | 13 | | 34 | 25 | | | 0.7 | 21815 | 1.0 |
A1196 | d | 78 | Neergaard Dal | 81.78512 | -26.66043 | 13.2 | | | | 47 | 11 | | | 2.5 | 645 | 0.1 |
A1195 | b | 190 | Neergaard Dal | 81.78532 | -26.66077 | 11.8 | | | | 57 | 31 | 6 | | 2.3 | 1081 | 0.4 |
A1196 | a | 54 | Neergaard Dal | 81.78512 | -26.66043 | 11.8 | | | | 33 | | | | 2.3 | 1115 | 0.1 |
A1196 | a | 173 | Neergaard Dal | 81.78512 | -26.66043 | 11.7 | | | | 34 | 4 | | | 2.8 | 918 | 0.1 |
A1198 | c | 246 | Discovery Zone | 81.95524 | -26.20146 | 11.2 | 311 | 43 | | 34 | 74 | | | 4.9 | 41940 | 1.3 |
A1196 | bag fines | 282 | Neergaard Dal | 81.78512 | -26.66043 | 10.9 | 14 | | 3 | | 8 | | 15 | 2.6 | 617 | 0.2 |
A1196 | bag fines | 283 | Neergaard Dal | 81.78512 | -26.66043 | 10.9 | 12 | | | 16 | 9 | | 13 | 2.2 | 522 | 0.2 |
A1196 | bag fines | 281 | Neergaard Dal | 81.78512 | -26.66043 | 10.7 | 12 | | | 13 | 8 | | | 2.3 | 386 | 0.2 |
A1196 | bag fines | 284 | Neergaard Dal | 81.78512 | -26.66043 | 10.6 | 14 | | 6 | | 7 | | 13 | 2.5 | 384 | 0.1 |
A1196 | b | 71 | Neergaard Dal | 81.78512 | -26.66043 | 10.6 | 5 | | | 45 | | 6 | | 2.6 | | 0.3 |
A1192 | a | 91 | Neergaard Dal | 81.78540 | -26.66103 | 10.5 | | | | 34 | 4 | | | 2.3 | 4935 | 0.1 |
A1199 | d | 213 | Discovery Zone | 81.95516 | -26.20024 | 10.3 | 249 | 75 | 6 | 28 | 140 | | 8 | 3.7 | 20881 | 4.1 |
A1197 | bag fragments | 267 | Discovery Zone | 81.95527 | -26.20158 | 10.1 | 191 | 15 | | 20 | 70 | | | 2.2 | 19484 | 1.6 |
A1215 | a | 154 | Discovery Zone | 81.95586 | -26.20112 | 9.7 | 11 | | | 13 | 3 | | | 0.4 | 13948 | 0.2 |
A1198 | a | 237 | Discovery Zone | 81.95524 | -26.20146 | 9.6 | 30 | 28 | | 21 | 11 | | | 0.3 | 15002 | 0.8 |
A1197 | d | 233 | Discovery Zone | 81.95527 | -26.20158 | 9.6 | 309 | 55 | | 18 | 252 | | | 2.7 | 35932 | 2.3 |
A1196 | a | 55 | Neergaard Dal | 81.78512 | -26.66043 | 9.3 | 5 | | | 49 | 3 | | | 1.4 | 10364 | 0.2 |
A1197 | bag fragments | 278 | Discovery Zone | 81.95527 | -26.20158 | 9.1 | 356 | 66 | | 40 | 212 | | | 1.9 | 31429 | 2.2 |
A1197 | bag fragments | 274 | Discovery Zone | 81.95527 | -26.20158 | 9.1 | 349 | 51 | 8 | 39 | 235 | | | 3.2 | 28251 | 2.0 |
A1196 | bag fines | 285 | Neergaard Dal | 81.78512 | -26.66043 | 9.0 | 12 | | 7 | | 7 | | 14 | 2.1 | 425 | 0.2 |
A1197 | b | 226 | Discovery Zone | 81.95527 | -26.20158 | 8.9 | 427 | 63 | 5 | 33 | 327 | | | 2.0 | 17594 | 1.2 |
A1196 | e | 82 | Neergaard Dal | 81.78512 | -26.66043 | 8.7 | 6 | | | 49 | 8 | 8 | | 3.0 | 535 | 0.1 |
A1197 | a | 225 | Discovery Zone | 81.95527 | -26.20158 | 8.5 | 242 | 24 | | 34 | 202 | | | 1.7 | 14413 | 1.4 |
A1200 | c | 132 | Discovery Zone | 81.95513 | -26.20054 | 8.4 | 30 | 13 | | 94 | 15 | | 6 | 3.2 | 15140 | 1.6 |
A1196 | bag fines | 280 | Neergaard Dal | 81.78512 | -26.66043 | 8.0 | 14 | | 3 | | 5 | | 9 | 3.2 | 92 | 0.1 |
A1195 | b | 193 | Neergaard Dal | 81.78532 | -26.66077 | 7.7 | | | | 67 | 11 | | | 1.9 | 671 | 0.2 |
A1196 | bag fines | 287 | Neergaard Dal | 81.78512 | -26.66043 | 7.6 | 8 | | | 12 | 6 | | | 2.5 | | 0.1 |
A1198 | a | 140 | Discovery Zone | 81.95524 | -26.20146 | 7.3 | 487 | 26 | | 29 | 96 | | | 2.3 | 15701 | 3.9 |
A1198 | b | 145 | Discovery Zone | 81.95524 | -26.20146 | 6.9 | 151 | 22 | | 17 | 83 | | | 0.8 | 15115 | 1.4 |
A1198 | a | 142 | Discovery Zone | 81.95524 | -26.20146 | 6.9 | 602 | 30 | 3 | 36 | 51 | | | 1.7 | 16747 | 3.3 |
A1199 | c | 209 | Discovery Zone | 81.95516 | -26.20024 | 6.8 | 63 | 41 | | 26 | 19 | | | 1.5 | 18992 | 2.4 |
A1199 | bag fines | 161 | Discovery Zone | 81.95516 | -26.20024 | 6.8 | 394 | 80 | | 36 | 303 | | | 2.8 | 4907 | 1.0 |
A1197 | bag fragments | 271 | Discovery Zone | 81.95527 | -26.20158 | 6.7 | 370 | 73 | | 47 | 166 | | | 3.8 | 17839 | 2.8 |
A1199 | bag fines | 300 | Discovery Zone | 81.95516 | -26.20024 | 6.7 | 453 | 85 | | 70 | 252 | | | 3.9 | 16046 | 2.3 |
A1199 | f | 220 | Discovery Zone | 81.95516 | -26.20024 | 6.6 | 4032 | 547 | 10 | 133 | 2523 | | | 16.0 | 20675 | 1.8 |
A1199 | bag fines | 302 | Discovery Zone | 81.95516 | -26.20024 | 6.6 | 450 | 86 | | 53 | 381 | 6 | | 3.7 | 14654 | 2.5 |
A1199 | bag fines | 307 | Discovery Zone | 81.95516 | -26.20024 | 6.5 | 564 | 99 | 6 | 58 | 469 | | | 4.0 | 11926 | 1.9 |
A1197 | b | 228 | Discovery Zone | 81.95527 | -26.20158 | 6.5 | 300 | 44 | 4 | 28 | 178 | | | 3.8 | 30506 | 3.2 |
A1198 | c | 244 | Discovery Zone | 81.95524 | -26.20146 | 6.5 | 527 | 201 | | 44 | 884 | | | 7.7 | 31343 | 1.5 |
A1196 | bag fines | 289 | Neergaard Dal | 81.78512 | -26.66043 | 6.2 | 12 | | 3 | 15 | 4 | | 19 | 2.5 | 294 | 0.1 |
A1198 | b | 147 | Discovery Zone | 81.95524 | -26.20146 | 6.2 | 39 | 6 | | 37 | 29 | | | 1.2 | 13529 | 2.2 |
A1199 | bag fines | 306 | Discovery Zone | 81.95516 | -26.20024 | 6.2 | 458 | 82 | | 61 | 266 | | | 3.1 | 16142 | 2.4 |
A1196 | a | 172 | Neergaard Dal | 81.78512 | -26.66043 | 6.1 | 6 | | | 42 | 24 | | | 2.0 | 6146 | 0.1 |
A1199 | bag fines | 304 | Discovery Zone | 81.95516 | -26.20024 | 6.1 | 465 | 93 | | 48 | 361 | | | 3.7 | 15924 | 2.7 |
A1197 | bag fragments | 263 | Discovery Zone | 81.95527 | -26.20158 | 6.0 | 93 | 44 | | 35 | 999 | | | 3.3 | 9049 | 4.0 |
A1198 | a | 139 | Discovery Zone | 81.95524 | -26.20146 | 5.9 | 473 | 12 | | 30 | 47 | | | 2.0 | 16066 | 2.7 |
A1197 | c | 232 | Discovery Zone | 81.95527 | -26.20158 | 5.9 | 225 | 10 | | 37 | 67 | | | 1.7 | 40735 | 1.2 |
A1196 | bag fines | 288 | Neergaard Dal | 81.78512 | -26.66043 | 5.6 | 10 | | 6 | 19 | 4 | | | 2.4 | | 0.1 |
A1199 | bag fines | 305 | Discovery Zone | 81.95516 | -26.20024 | 5.5 | 445 | 70 | | 43 | 252 | | | 2.9 | 13941 | 2.6 |
A1199 | bag fines | 309 | Discovery Zone | 81.95516 | -26.20024 | 5.5 | 421 | 71 | | 45 | 226 | | | 2.9 | 13615 | 2.3 |
A1198 | b | 241 | Discovery Zone | 81.95524 | -26.20146 | 5.5 | 253 | 20 | | 15 | 45 | | | 0.7 | 15414 | 1.4 |
A1198 | a | 138 | Discovery Zone | 81.95524 | -26.20146 | 5.5 | 93 | 5 | | 21 | 12 | | | 1.2 | 14625 | 1.0 |
A1197 | bag fragments | 260 | Discovery Zone | 81.95527 | -26.20158 | 5.4 | 64 | 4 | | 15 | 7 | | | 4.1 | 12619 | 0.5 |
A1198 | a | 141 | Discovery Zone | 81.95524 | -26.20146 | 5.3 | 434 | 50 | | 37 | 78 | | | 2.1 | 14616 | 3.3 |
A1199 | bag fines | 303 | Discovery Zone | 81.95516 | -26.20024 | 5.1 | 308 | 60 | | 41 | 217 | | | 2.9 | 9482 | 1.8 |
A1199 | bag fines | 163 | Discovery Zone | 81.95516 | -26.20024 | 4.9 | 341 | 71 | | 26 | 286 | | | 4.0 | 11192 | 2.6 |
A1197 | bag fragments | 276 | Discovery Zone | 81.95527 | -26.20158 | 4.9 | 347 | 19 | | 29 | 44 | | | 1.2 | 17476 | 1.1 |
A1198 | d | 248 | Discovery Zone | 81.95524 | -26.20146 | 4.9 | 30 | 19 | | 20 | 29 | | | 2.0 | 16755 | 2.3 |
A1197 | bag fines | 296 | Discovery Zone | 81.95527 | -26.20158 | 4.8 | 142 | 39 | | 38 | 443 | | | 3.3 | 7003 | 3.3 |
A1195 | b | 192 | Neergaard Dal | 81.78532 | -26.66077 | 4.8 | | | | 37 | | | | 1.3 | 4949 | 0.2 |
A1194 | a | 106 | Neergaard Dal | 81.78535 | -26.66126 | 4.6 | 7 | | | 48 | | 14 | | 4.8 | 2248 | 0.1 |
A1196 | d | 80 | Neergaard Dal | 81.78512 | -26.66043 | 4.6 | | | | 39 | 2 | | | 2.7 | 1210 | 0.1 |
A1196 | b | 68 | Neergaard Dal | 81.78512 | -26.66043 | 4.6 | | 5 | | 53 | 7 | | | 3.3 | | 0.1 |
A1199 | bag fines | 160 | Discovery Zone | 81.95516 | -26.20024 | 4.5 | 267 | 91 | | 26 | 348 | | | 3.2 | 4014 | 0.8 |
A1196 | c | 74 | Neergaard Dal | 81.78512 | -26.66043 | 4.5 | 4 | | | 44 | | | | 3.9 | 845 | 0.1 |
A1198 | b | 146 | Discovery Zone | 81.95524 | -26.20146 | 4.5 | 115 | | | 24 | 14 | | | 1.9 | 12980 | 1.2 |
A1198 | b | 243 | Discovery Zone | 81.95524 | -26.20146 | 4.5 | 18 | 5 | | 17 | 9 | | | 0.3 | 12310 | 0.7 |
A1197 | bag fines | 297 | Discovery Zone | 81.95527 | -26.20158 | 4.5 | 181 | 41 | | 42 | 479 | | | 2.9 | 8982 | 3.5 |
A1197 | a | 224 | Discovery Zone | 81.95527 | -26.20158 | 4.5 | 34 | 48 | | 26 | 120 | | | 2.0 | 12469 | 2.2 |
A1200 | a | 129 | Discovery Zone | 81.95513 | -26.20054 | 4.4 | 39 | 18 | | 32 | 184 | | | 5.5 | 17149 | 3.1 |
A1197 | bag fines | 292 | Discovery Zone | 81.95527 | -26.20158 | 4.4 | 124 | 42 | | | 401 | | 8 | 3.3 | 8146 | 4.0 |
A1197 | bag fines | 298 | Discovery Zone | 81.95527 | -26.20158 | 4.3 | 152 | 31 | | 34 | 355 | | | 3.4 | 8536 | 3.8 |
A1197 | bag fines | 295 | Discovery Zone | 81.95527 | -26.20158 | 4.3 | 158 | 38 | | 36 | 450 | | | 3.2 | 7437 | 3.2 |
A1198 | d | 247 | Discovery Zone | 81.95524 | -26.20146 | 4.2 | 16 | 32 | | 32 | 18 | | | 1.9 | 13393 | 1.5 |
A1197 | bag fragments | 269 | Discovery Zone | 81.95527 | -26.20158 | 4.1 | 35 | 28 | | 24 | 30 | | | 0.8 | 26499 | 1.3 |
A1199 | bag fines | 301 | Discovery Zone | 81.95516 | -26.20024 | 4.1 | 342 | 68 | 3 | 53 | 155 | | | 3.1 | 13671 | 3.4 |
A1198 | d | 249 | Discovery Zone | 81.95524 | -26.20146 | 4.1 | 71 | 28 | | 30 | 112 | | | 2.7 | 16299 | 3.6 |
A1199 | bag fines | 162 | Discovery Zone | 81.95516 | -26.20024 | 4.1 | 251 | 34 | 4 | 46 | 84 | | | 2.4 | 12873 | 1.9 |
A1197 | bag fines | 291 | Discovery Zone | 81.95527 | -26.20158 | 4.0 | 141 | 40 | | 48 | 360 | | | 2.9 | 9026 | 3.7 |
A1197 | bag fragments | 265 | Discovery Zone | 81.95527 | -26.20158 | 4.0 | 255 | 24 | | 58 | 325 | | | 2.8 | 8042 | 3.7 |
A1197 | bag fines | 293 | Discovery Zone | 81.95527 | -26.20158 | 4.0 | 128 | 30 | | 26 | 396 | | | 3.1 | 7736 | 3.6 |
A1196 | a | 63 | Neergaard Dal | 81.78512 | -26.66043 | 4.0 | 8 | | | | | | | 2.6 | | 0.0 |
A1197 | bag fragments | 266 | Discovery Zone | 81.95527 | -26.20158 | 3.6 | 96 | 30 | | 28 | 404 | | | 3.5 | 8644 | 4.1 |
A1197 | bag fines | 290 | Discovery Zone | 81.95527 | -26.20158 | 3.6 | 116 | 31 | | 27 | 309 | | | 2.9 | 6734 | 3.2 |
A1197 | b | 229 | Discovery Zone | 81.95527 | -26.20158 | 3.6 | 243 | 16 | | 37 | 144 | | | 2.3 | 16940 | 1.3 |
A1199 | bag fines | 164 | Discovery Zone | 81.95516 | -26.20024 | 3.6 | 340 | 96 | 5 | 33 | 193 | | | 4.0 | 14344 | 2.9 |
A1195 | c | 194 | Neergaard Dal | 81.78532 | -26.66077 | 3.5 | 7 | 5 | | 34 | 19 | | | 3.8 | 338 | 0.5 |
A1197 | bag fines | 299 | Discovery Zone | 81.95527 | -26.20158 | 3.5 | 138 | 36 | | 51 | 390 | 6 | | 2.7 | 6819 | 3.7 |
A1197 | bag fines | 294 | Discovery Zone | 81.95527 | -26.20158 | 3.4 | 125 | 31 | | 42 | 318 | | | 2.6 | 8384 | 3.3 |
A1196 | d | 79 | Neergaard Dal | 81.78512 | -26.66043 | 3.4 | 4 | 5 | | 40 | 3 | 4 | | 3.0 | 131 | 0.1 |
A1196 | a | 175 | Neergaard Dal | 81.78512 | -26.66043 | 3.4 | 6 | | | 35 | 3 | | | 1.9 | 670 | 0.1 |
A1197 | bag fragments | 277 | Discovery Zone | 81.95527 | -26.20158 | 3.3 | 32 | 9 | | 18 | 40 | | | 0.9 | 14096 | 1.2 |
A1200 | c | 133 | Discovery Zone | 81.95513 | -26.20054 | 3.3 | 53 | 19 | | 24 | 51 | | | 4.7 | 30081 | 3.6 |
A1198 | b | 242 | Discovery Zone | 81.95524 | -26.20146 | 3.3 | 89 | 7 | | 10 | 26 | | | 0.5 | 9687 | 0.9 |
A1193 | b | 100 | Neergaard Dal | 81.78541 | -26.66100 | 3.3 | 4 | | | 55 | | | | 3.8 | 5401 | 0.0 |
A1199 | c | 208 | Discovery Zone | 81.95516 | -26.20024 | 3.3 | 29 | 23 | | 16 | 11 | | | 1.2 | 15240 | 1.9 |
A1196 | a | 52 | Neergaard Dal | 81.78512 | -26.66043 | 3.1 | | | | 32 | 5 | | | 2.7 | 1442 | 0.1 |
A1199 | bag fines | 308 | Discovery Zone | 81.95516 | -26.20024 | 3.1 | 349 | 67 | 4 | 29 | 212 | | | 2.7 | 11949 | 3.0 |
A1195 | a | 181 | Neergaard Dal | 81.78532 | -26.66077 | 3.0 | | 5 | | 44 | | | | 4.9 | 378 | 0.2 |
A1194 | c | 118 | Neergaard Dal | 81.78535 | -26.66126 | 3.0 | | | | 42 | | | | 3.9 | 748 | 0.1 |
A1197 | bag fragments | 272 | Discovery Zone | 81.95527 | -26.20158 | 2.8 | 44 | 34 | | 26 | 49 | | | 2.2 | 14243 | 3.0 |
A1197 | bag fines | 165 | Discovery Zone | 81.95527 | -26.20158 | 2.8 | 122 | 17 | | 29 | 153 | | | 2.0 | 4382 | 1.3 |
A1195 | b | 191 | Neergaard Dal | 81.78532 | -26.66077 | 2.7 | | 6 | | 53 | | 6 | | 4.2 | 285 | 0.2 |
A1192 | a | 84 | Neergaard Dal | 81.78540 | -26.66103 | 2.6 | | | | 21 | | | | 0.5 | 345 | 0.1 |
A1196 | a | 61 | Neergaard Dal | 81.78512 | -26.66043 | 2.4 | | | | 56 | | | | 2.5 | | 0.2 |
A1196 | b | 67 | Neergaard Dal | 81.78512 | -26.66043 | 2.3 | | | | 42 | | | | 2.8 | 383 | 0.1 |
A1197 | bag fragments | 273 | Discovery Zone | 81.95527 | -26.20158 | 2.2 | 145 | 12 | | 32 | 96 | | | 2.1 | 12243 | 2.7 |
A1197 | a | 222 | Discovery Zone | 81.95527 | -26.20158 | 2.0 | 121 | 34 | | 32 | 379 | | | 3.8 | 12421 | 5.6 |
A1200 | c | 134 | Discovery Zone | 81.95513 | -26.20054 | 2.0 | 98 | 23 | | 21 | 17 | | | 3.5 | 8171 | 2.3 |
A1197 | bag fragments | 261 | Discovery Zone | 81.95527 | -26.20158 | 1.9 | 54 | 15 | | 26 | 121 | | | 1.6 | 9983 | 2.5 |
A1196 | c | 73 | Neergaard Dal | 81.78512 | -26.66043 | 1.9 | | | | 36 | | | | 3.3 | 175 | 0.2 |
A1192 | a | 92 | Neergaard Dal | 81.78540 | -26.66103 | 1.9 | | 6 | | 41 | | 5 | | 4.7 | 241 | 0.1 |
A1197 | bag fragments | 270 | Discovery Zone | 81.95527 | -26.20158 | 1.8 | 51 | 10 | | 26 | 71 | | | 2.3 | 13100 | 1.7 |
A1200 | d | 135 | Discovery Zone | 81.95513 | -26.20054 | 1.8 | 43 | 30 | | 39 | 242 | | | 4.9 | 13455 | 4.0 |
A1195 | c | 195 | Neergaard Dal | 81.78532 | -26.66077 | 1.8 | | 3 | | 26 | | | | 3.0 | 493 | 0.6 |
A1197 | bag fragments | 262 | Discovery Zone | 81.95527 | -26.20158 | 1.8 | 59 | 13 | | 21 | 41 | | | 0.6 | 8743 | 0.5 |
A1193 | b | 102 | Neergaard Dal | 81.78541 | -26.66100 | 1.8 | 4 | 3 | | 41 | | | | 4.0 | 309 | 0.1 |
A1196 | a | 62 | Neergaard Dal | 81.78512 | -26.66043 | 1.7 | | 4 | | 47 | | | | 4.0 | 459 | 0.5 |
A1199 | d | 211 | Discovery Zone | 81.95516 | -26.20024 | 1.7 | 500 | 76 | 6 | 18 | 238 | | | 5.8 | 11004 | 4.8 |
A1197 | bag fragments | 275 | Discovery Zone | 81.95527 | -26.20158 | 1.7 | 35 | | | 12 | 21 | | | 0.7 | 14421 | 1.1 |
A1197 | bag fragments | 259 | Discovery Zone | 81.95527 | -26.20158 | 1.7 | 22 | 14 | | 19 | 52 | | | 1.6 | 10135 | 3.0 |
A1198 | a | 238 | Discovery Zone | 81.95524 | -26.20146 | 1.7 | 18 | | | 24 | 27 | | | 0.5 | 11296 | 1.5 |
A1198 | a | 236 | Discovery Zone | 81.95524 | -26.20146 | 1.5 | 54 | | | 23 | 8 | | | 0.3 | 3162 | 0.5 |
A1198 | c | 245 | Discovery Zone | 81.95524 | -26.20146 | 1.4 | 111 | 26 | | 13 | 37 | | | 3.9 | 11558 | 1.8 |
A1200 | d | 136 | Discovery Zone | 81.95513 | -26.20054 | 1.4 | 65 | 36 | | 45 | 248 | | | 4.2 | 11660 | 4.2 |
A1198 | b | 149 | Discovery Zone | 81.95524 | -26.20146 | 1.3 | 60 | 28 | | 14 | 16 | | | 0.5 | 3854 | 1.3 |
A1198 | a | 143 | Discovery Zone | 81.95524 | -26.20146 | 1.3 | 95 | 5 | | 18 | 20 | | | 0.4 | 7991 | 1.2 |
A1199 | c | 207 | Discovery Zone | 81.95516 | -26.20024 | 1.3 | 21 | 19 | | 20 | 13 | | | 1.4 | 16009 | 2.9 |
A1196 | a | 53 | Neergaard Dal | 81.78512 | -26.66043 | 1.3 | | | | 33 | | | | 2.0 | 8814 | 0.2 |
A1197 | bag fragments | 268 | Discovery Zone | 81.95527 | -26.20158 | 1.3 | 27 | | | 18 | 15 | | | 0.8 | 13616 | 1.3 |
A1197 | bag fragments | 264 | Discovery Zone | 81.95527 | -26.20158 | 1.3 | 23 | 12 | | 17 | 122 | | | 1.4 | 7736 | 4.1 |
A1192 | a | 85 | Neergaard Dal | 81.78540 | -26.66103 | 1.2 | | | | | | | | 1.7 | | 0.1 |
A1200 | a | 128 | Discovery Zone | 81.95513 | -26.20054 | 1.2 | 29 | 10 | | 25 | 72 | | | 4.4 | 10670 | 2.8 |
A1198 | b | 148 | Discovery Zone | 81.95524 | -26.20146 | 1.2 | 84 | | | 20 | 10 | | | 0.9 | 4711 | 1.5 |
A1199 | e | 218 | Discovery Zone | 81.95516 | -26.20024 | 1.1 | 42 | 21 | | 15 | 18 | | | 1.5 | 6681 | 3.8 |
A1199 | e | 215 | Discovery Zone | 81.95516 | -26.20024 | 1.1 | 26 | 15 | | 17 | 15 | | | 1.2 | 13821 | 3.5 |
A1196 | a | 59 | Neergaard Dal | 81.78512 | -26.66043 | 1.1 | 4 | 4 | | 20 | | | | 1.8 | 135 | 0.3 |
A1195 | c | 197 | Neergaard Dal | 81.78532 | -26.66077 | 1.1 | | | | 30 | 28 | | | 0.7 | | 0.0 |
A1215 | a | 251 | Discovery Zone | 81.95586 | -26.20112 | 1.0 | 51 | | | 16 | 11 | | | 0.5 | 3436 | 0.3 |
A1192 | a | 178 | Neergaard Dal | 81.78540 | -26.66103 | 1.0 | | | | 37 | 3 | | | 2.6 | 467 | 0.1 |
A1196 | bag fines | 166 | Neergaard Dal | 81.78512 | -26.66043 | 0.9 | 5 | | | 40 | 3 | | | 0.8 | 1911 | 0.6 |
A1197 | a | 223 | Discovery Zone | 81.95527 | -26.20158 | 0.9 | 139 | 24 | | 33 | 360 | | | 3.2 | 4300 | 5.3 |
A1200 | a | 127 | Discovery Zone | 81.95513 | -26.20054 | 0.9 | 21 | 7 | | 18 | 38 | | | 2.9 | 7707 | 3.5 |
A1215 | a | 155 | Discovery Zone | 81.95586 | -26.20112 | 0.9 | 31 | | | 9 | 6 | | | 0.4 | 2352 | 0.3 |
A1198 | a | 240 | Discovery Zone | 81.95524 | -26.20146 | 0.9 | 81 | 6 | | 16 | 18 | | | 0.3 | 4497 | 1.1 |
A1199 | e | 217 | Discovery Zone | 81.95516 | -26.20024 | 0.9 | 44 | 13 | | 15 | 23 | | | 1.2 | 9321 | 4.0 |
A1192 | a | 90 | Neergaard Dal | 81.78540 | -26.66103 | 0.9 | | | | 22 | | | | 0.2 | 184 | 0.1 |
A1196 | b | 66 | Neergaard Dal | 81.78512 | -26.66043 | 0.8 | | | | 47 | | | | 0.9 | 4958 | 0.1 |
A1200 | a | 126 | Discovery Zone | 81.95513 | -26.20054 | 0.8 | 26 | 9 | | 30 | 89 | | | 3.4 | 9387 | 2.6 |
A1192 | a | 89 | Neergaard Dal | 81.78540 | -26.66103 | 0.8 | | | | 25 | 2 | | | 2.4 | 1526 | 0.1 |
A1198 | a | 144 | Discovery Zone | 81.95524 | -26.20146 | 0.8 | 39 | 4 | | 11 | 8 | | | 0.5 | 6113 | 1.1 |
A1199 | c | 125 | Discovery Zone | 81.95516 | -26.20024 | 0.8 | 20 | 38 | | 20 | 7 | | | 1.7 | 9335 | 4.3 |
A1196 | a | 56 | Neergaard Dal | 81.78512 | -26.66043 | 0.8 | | | | 14 | | | | 0.2 | 531 | 0.1 |
A1199 | e | 216 | Discovery Zone | 81.95516 | -26.20024 | 0.7 | 34 | 11 | | 18 | 22 | | | 1.2 | 7482 | 4.0 |
A1199 | c | 206 | Discovery Zone | 81.95516 | -26.20024 | 0.7 | 18 | 46 | | 11 | 12 | | | 1.4 | 8598 | 4.4 |
A1196 | e | 81 | Neergaard Dal | 81.78512 | -26.66043 | 0.7 | 6 | | | 48 | | | | 3.5 | 175 | 0.2 |
A1194 | a | 107 | Neergaard Dal | 81.78535 | -26.66126 | 0.6 | | | | 50 | | | | 5.0 | 130 | 0.1 |
A1196 | a | 174 | Neergaard Dal | 81.78512 | -26.66043 | 0.6 | 3 | | | | | | | 0.5 | 842 | 0.1 |
A1197 | d | 234 | Discovery Zone | 81.95527 | -26.20158 | 0.6 | 99 | 19 | 4 | 23 | 63 | | 4 | 2.4 | 8411 | 1.6 |
A1192 | a | 83 | Neergaard Dal | 81.78540 | -26.66103 | 0.5 | | | | 18 | 2 | | | 1.7 | 413 | 0.2 |
A1196 | a | 58 | Neergaard Dal | 81.78512 | -26.66043 | 0.5 | | | | 27 | | | | 2.3 | | 0.1 |
A1197 | b | 227 | Discovery Zone | 81.95527 | -26.20158 | 0.5 | 105 | 8 | | 23 | 24 | | | 1.6 | 3683 | 1.8 |
A1192 | a | 87 | Neergaard Dal | 81.78540 | -26.66103 | 0.5 | | | | | | | | 1.2 | | 0.0 |
A1215 | a | 253 | Discovery Zone | 81.95586 | -26.20112 | 0.4 | 9 | | | 9 | 2 | | | 0.2 | 3195 | 0.3 |
A1215 | a | 156 | Discovery Zone | 81.95586 | -26.20112 | 0.4 | | | | 18 | | | | 0.4 | 3391 | 1.0 |
A1200 | b | 130 | Discovery Zone | 81.95513 | -26.20054 | 0.3 | 3 | 6 | | 22 | 44 | | | 3.4 | 5121 | 4.2 |
A1196 | a | 60 | Neergaard Dal | 81.78512 | -26.66043 | 0.3 | | | | 24 | | | | 1.6 | 466 | 0.1 |
A1195 | a | 180 | Neergaard Dal | 81.78532 | -26.66077 | 0.3 | | | | 32 | | | | 2.7 | 626 | 0.2 |
A1192 | a | 86 | Neergaard Dal | 81.78540 | -26.66103 | 0.3 | | | | | | | | 0.3 | 404 | 0.1 |
A1195 | b | 188 | Neergaard Dal | 81.78532 | -26.66077 | 0.3 | | | | 38 | | | | 3.3 | 1172 | 0.4 |
A1195 | a | 183 | Neergaard Dal | 81.78532 | -26.66077 | 0.3 | 5 | | | 32 | | | | 3.7 | 328 | 0.1 |
A1215 | a | 250 | Discovery Zone | 81.95586 | -26.20112 | 0.3 | 8 | | | 9 | 2 | | | 0.2 | 1374 | 0.3 |
A1192 | a | 176 | Neergaard Dal | 81.78540 | -26.66103 | 0.2 | | | | 24 | | | | 1.0 | 675 | 0.3 |
A1193 | a | 93 | Neergaard Dal | 81.78541 | -26.66100 | 0.2 | | 4 | | 32 | | 5 | | 4.2 | 538 | 0.2 |
A1200 | b | 131 | Discovery Zone | 81.95513 | -26.20054 | 0.2 | 5 | 6 | | 18 | 26 | | | 2.0 | 1474 | 5.0 |
A1195 | a | 185 | Neergaard Dal | 81.78532 | -26.66077 | 0.2 | | | | | 4 | | | 3.1 | 896 | 0.3 |
A1192 | a | 177 | Neergaard Dal | 81.78540 | -26.66103 | 0.2 | | | | 13 | | | | 0.7 | 1583 | 0.5 |
A1195 | b | 187 | Neergaard Dal | 81.78532 | -26.66077 | 0.2 | | | | 55 | | | | 0.2 | 3553 | 0.1 |
A1193 | a | 96 | Neergaard Dal | 81.78541 | -26.66100 | 0.1 | | | | 31 | | | | 5.3 | 309 | 0.2 |
A1215 | a | 252 | Discovery Zone | 81.95586 | -26.20112 | 0.1 | | | | 15 | | | | 0.1 | 1997 | 0.3 |
A1195 | a | 184 | Neergaard Dal | 81.78532 | -26.66077 | 0.1 | | | | 36 | 2 | | | 3.7 | 402 | 0.1 |
A1195 | a | 179 | Neergaard Dal | 81.78532 | -26.66077 | 0.1 | 6 | | | 21 | | | | 4.1 | 569 | 0.3 |
A1193 | b | 101 | Neergaard Dal | 81.78541 | -26.66100 | 0.1 | 5 | | | 25 | | | | 4.2 | 96 | 0.1 |
A1215 | a | 151 | Discovery Zone | 81.95586 | -26.20112 | 0.1 | | | | 15 | | | | 0.1 | 1000 | 0.3 |
A1195 | a | 186 | Neergaard Dal | 81.78532 | -26.66077 | 0.1 | 4 | 9 | | 36 | | | | 9.6 | 1249 | 0.2 |
A1193 | c | 103 | Neergaard Dal | 81.78541 | -26.66100 | 0.1 | 5 | 6 | | 50 | | 6 | | 8.6 | 774 | 0.5 |
A1195 | a | 182 | Neergaard Dal | 81.78532 | -26.66077 | 0.1 | | | | 41 | | 4 | | 4.7 | 227 | 0.1 |
A1195 | c | 196 | Neergaard Dal | 81.78532 | -26.66077 | 0.1 | | | | 33 | 5 | 10 | | 4.5 | 1198 | 0.2 |
A1194 | c | 117 | Neergaard Dal | 81.78535 | -26.66126 | 0.0 | | | | 35 | 2 | | | 5.6 | 167 | 0.1 |
A1193 | a | 98 | Neergaard Dal | 81.78541 | -26.66100 | 0.0 | | | | 55 | | | | 7.3 | 1006 | 0.4 |
A1194 | b | 115 | Neergaard Dal | 81.78535 | -26.66126 | 0.0 | | 6 | | 34 | | | | 8.4 | 342 | 0.1 |
A1193 | a | 94 | Neergaard Dal | 81.78541 | -26.66100 | 0.0 | | 6 | | 39 | | | | 3.0 | 804 | 0.3 |
A1193 | a | 95 | Neergaard Dal | 81.78541 | -26.66100 | 0.0 | | | | 20 | | | | 4.4 | 321 | 0.1 |
A1191 | c | 121 | Neergaard Dal | 81.78530 | -26.66067 | 0.0 | | 10 | | 49 | | | | 9.1 | 2010 | 0.3 |
A1193 | c | 104 | Neergaard Dal | 81.78541 | -26.66100 | 0.0 | | 4 | | 55 | | | | 4.7 | 206 | 0.2 |
A1194 | a | 105 | Neergaard Dal | 81.78535 | -26.66126 | 0.0 | 5 | 3 | | 32 | | | | 5.2 | 141 | 0.0 |
A1191 | a | 119 | Neergaard Dal | 81.78530 | -26.66067 | 0.0 | | 6 | | 16 | | | | 6.7 | 937 | 0.0 |
A1191 | b | 120 | Neergaard Dal | 81.78530 | -26.66067 | 0.0 | | | | 42 | | | | 3.0 | 1800 | 0.2 |
A1193 | b | 99 | Neergaard Dal | 81.78541 | -26.66100 | 0.0 | 4 | 7 | | 46 | | | | 9.9 | 490 | 0.1 |
A1193 | a | 97 | Neergaard Dal | 81.78541 | -26.66100 | 0.0 | | 8 | | 29 | | 5 | | 7.3 | 342 | 0.1 |
A1191 | d | 122 | Neergaard Dal | 81.78530 | -26.66067 | 0.0 | | 13 | | 35 | | | | 10.5 | 680 | 0.5 |
A1194 | b | 116 | Neergaard Dal | 81.78535 | -26.66126 | 0.0 | 3 | | | 41 | 3 | 8 | | 5.0 | 263 | 0.1 |
A1192 | a | 88 | Neergaard Dal | 81.78540 | -26.66103 | 0.0 | 4 | 11 | | 31 | | | | 11.9 | 218 | 0.1 |
A1191 | e | 123 | Neergaard Dal | 81.78530 | -26.66067 | 0.0 | | | | 46 | | | | 7.0 | 1574 | 0.5 |
A1191 | f | 124 | Neergaard Dal | 81.78530 | -26.66067 | 0.0 | | | | 39 | | | | 5.8 | | 0.0 |
Note: Values over 1% Cu and 200 g/t Ag are highlighted in green. A review of the quantum of the other elements, and correlation analysis with economically interesting elements was performed. The elements that are not correlated and have background values are omitted from this table to make the data easier for handle for the reader.
JORC Table 1, section 2: Reporting of Exploration Results | |
Criteria | Arctic Rift Copper project |
Mineral tenement and land tenure status | The Arctic Rift Copper project ('ARC') comprises a single Special Exploration Licence ('MEL-S' 2021-07). The spatial area of the application is 5,774km2, the boundary of which is defined by the points: 82°3'N, 29°18'W 81°35'N, 26°8'W 82°3'N, 25°41'W 81°30'N, 26°8'W 82°0'N, 25°41'W 81°30'N, 26°54'W 82°0'N, 25°43'W 81°25'N, 26°54'W 81°59'N, 25°43'W 81°25'N, 28°20'W 81°59'N, 25°44'W 81°21'N, 28°20'W 81°58'N, 25°44'W 81°21'N, 29°35'W 81°58'N, 25°46'W 81°19'N, 29°35'W 81°56'N, 25°46'W 81°19'N, 31°0'W 81°56'N, 25°48'W 81°27'N, 31°0'W 81°55'N, 25°48'W 81°27'N, 31°42'W 81°55'N, 25°50'W 81°34'N, 31°42'W 81°53'N, 25°50'W 81°34'N, 32°7'W 81°53'N, 25°52'W 81°51'N, 32°7'W 81°50'N, 25°52'W 81°51'N, 31°0'W 81°50'N, 25°54'W 81°54'N, 31°0'W 81°46'N, 25°54'W 81°54'N, 30°18'W 81°46'N, 25°55'W 81°58'N, 30°18'W 81°35'N, 25°55'W 81°58'N, 29°18'W
An MEL-S confers an exclusive right to explore for minerals for three years at a reduced holding cost, provided each licence covers more than 1,000km2. After three years, the holder of Special Exploration Licence has the right to convert the area, whole or in part, to conventional Exploration Licences. Due to the Coronavirus pandemic, all licence obligations in Greenland were paused until the end of 2021, such that the MEL-S can convert to a normal licence at the end of 2024.
The minimum expenditure obligation for a MEL-S is DKK500/km2 indexed to Danish CPI as of January 1992. The Company estimates the expenditure requirement in the base case will be approximately AUD1,080,000 per annum. However, the Government waived all expenditure obligations for 2020 and 2021, and as such, no holding cost of the licence will crystallise until 31 December 2022. The obligation for 2022 will be calculated on 1 January 2023 based on the area under licence on the preceding day. Expenditure requirements for 2022 have been reduced by 50% due to the coronavirus pandemic. The licence is currently in credit due to expenditure in 2021. Expenditure above the minimum regulatory requirement is carried forward for a maximum of three years. ARC is in good standing and the Company currently owns 51% of the licence.
There are no third-party royalties or other rights relating to ARC. |
Exploration done by other parties | North Greenland was first commercially explored in 1969 and 1972, which identified native copper and copper sulphides in eastern North Greenland. It wasn't until 1979 and 1980 that more substantive work was performed, this time by the Government. ARC was subject to commercial exploration by Avannaa Resources Limited ('Avannaa') in 2010 and 2011. In its first year, Avannaa focussed its work on a small area in the northern part of the licence area known as Neergaard North. This work focussed on historical Government and academic work that had identified highly anomalous copper mineralisation. In 2010, the work included geochemical soil sampling, rock chipping and trenching of high-grade material associated with NW-SE trending fault breccias. Based on the success of the 2010 program, Avannaa undertook a much larger regional reconnaissance program in 2011. This program involved a heli-supported geochemical sampling program over a large area designed to test the copper prospectivity of various stratigraphic positions; as well as extending the length of the 'Discovery Zone' identified in 2010. Both aspects of this program were successful in that the Discovery Zone was shown to have a minimum strike length of 2km before disappearing undercover. Certain stratigraphic horizons show copper anomalism over a significant lateral extent. However, much of Avannaa's work was located to the southeast of the ARC and is now located in a Government-mandated no-go zone for mineral exploration. |
Geology | ARC contains a sequence of Mesoproterozoic-aged sandstone-dominated sediments belonging to the Independence Fjord Basin, that are intruded by highly altered dolerites and overlain by 1.2km of Mesoproterozoic-aged flood basalts ('Zig-Zag Fm' basalts). The basalts are overlain by 1.1km of Neoproterozoic-aged (1,000M to 541M years ago) clastic and carbonate sediments belonging to the Hagen Fjord Group. The lower portion of the Hagen Fjord Group is dominated by sandstones and siltstones, and the upper part by limestone and dolomites. Based on stream sediment samples, the iron oxide minerals switch from magnetite to the east of ARC, to haematite within ARC, which reflects a change in fluid oxidation state (from reduced to oxidised). Fluid flow is from east to west which implies that oxidation is a component of the copper dropping out of the solution. The oxidation of a reduced fluid is consistent with the chemistry required to form native copper, such as that observed in ARC. The metamorphic grade of the Zig-Zag Fm basalts is of the zeolite facies, and the Hagen Fjord Group sediments show lower grade metamorphism. There is adequate preservation aside from mechanical erosion.
Commercially interesting copper mineralisation occurs in the basalts and Hagen Fjord Group sediments. The basalts are known to contain in situ native copper, and native copper is found extensively in the surrounding drainage systems. Significantly, the native copper specimens recovered by the Government in 1979 and 1994, and by Avannaa in 2010 weigh up to 1kg. These large native copper specimens likely originate from amygdales (gas voids) in the basalt, although native copper occurring in faults is also known to occur within ARC. Greenfields considers that the age, setting, and mineral composition make the Zig-Zag Fm copper analogous to the copper deposits of the Michigan Upper (Keweenaw) Peninsula and a primary source of copper for the anomalies reported in the overlying sediments. The fault breccias that transect the basalts and Neoproterozoic sediments are Greenfields interprets these to represent fluid pathways as there are zones of intense potassium alteration within the surrounding quartz-dominated sedimentary rocks. These breccias are up to 25m wide and show copper mineralisation. The chalcocite, bornite and chalcopyrite copper-bearing minerals are significant as they demonstrate that sulphur has been added into a previously sulphur-undersaturated system. A source of sulphur is considered an important factor in the sediment-hosted copper 'deposit model'. Other important components of the deposit model are also reported, including pseudomorphed gypsum (a source of sulphur, and copper mobilising salts), hydrogeologic seals, and contrasting oxidation states. Copper sulphides occur in the predicted geological lithological settings. The highest copper grades are near geophysical gravity, magnetic and electromagnetic anomalies. The ~640 km2 area of geophysical and geochemical anomalism is dubbed the Minik Singularity.
The age of the known mineralisation concerns at least two episodes. Greenfields identifies the Elzevirian Orogeny (c. 1,250Ma) as the likely event associated with the native copper mineralisation in the basalts. However, the Neoproterozoic-aged sediment-hosted copper sulphides demonstrate a second mineralising event related to the waning Caledonian Orogeny (c. 390 to 380 Ma). The Elzevirian and Caledonian orogenies have a similar orientation. The c. 385 maximum age is supported by the absence of mineralisation known to be younger than the Silurian Period (443.8 Ma to 419.2 Ma). The Silurian is associated with the formation of the Citronen zinc deposit, currently licenced by Ironbark Zinc Ltd. Greenfields considers Citronen and ARC's copper sulphides to have formed due to the same event. The known copper and zinc, combined with Greenfields interpreted geological history, geochronology, and hydrothermal fluid temperatures, to define the +60,000km2 Kiffaanngissuseq Metallogenic Province.
The two hydrothermal events that Greenfields interprets to have created the Kiffaanngissuseq Metallogenic Province are distinctly different. Greenfields considers that the Elzevirian-aged fluids were chemically reduced but enriched in cerium. This cerium may have triggered anoxic oxidation of the copper-bearing titanomagnetite minerals. This interpretation is consistent with the observation at Astrup Anomaly, where the sedimentary rocks underneath the mafic appear to be chemically reduced (grey), whereas above the mafic they are oxidised. This implies that the reduced Elzevirian hydrothermal fluids that emanated from deeper underground and cerium bearing and quite vigorous in their interaction with the mafic rock to produce the intense iron-oxide staining above it. By comparison, the younger Caledonian hydrothermal fluids may have been oxidised, as at the Discovery Zone there is evidence that the fluids were reduced by pyrite, resulting in the precipitation of copper sulphides.
An interactive Government portal that contains the geology and supporting reports can be accessed via: http://www.greenmin.gl/home.seam . A fully referenced Technical Assessment Report on ARC, can be accessed at http://dx.doi.org/10.13140/RG.2.2.18610.84161 . |
Drill hole information | No drilling has ever occurred within the ARC or in the surrounding area. |
Data aggregation methods | Data aggregation was performed. For all samples, multiple pXRF readings were taken, and aggregated using medians, to reduce the inaccuracy associated with the small pXRF view window. |
Relationship between mineralisation width and intercept lengths. | The pXRF was performed on outcropping mineralisation. The mineralisation at Neergaard Dal and the Discovery Zone is hosted within steeply dipping faults (as expressed at surface). No transects were performed. The reported results are based on spot sampling of insitu material (Discovery Zone) and proximal scree (Neergaard Dal). All the samples collected weighed more than 1kg, with some being closer to 10kg. |
Diagrams | All relevant maps are presented in the main body of this document, with additional tables and figures available in the Technical Assessment Report. |
Balanced reporting | The Company has sourced and reasonably presented all the results. The results are presented statistically as well as graphically so that the reader can use these to make a balanced assessment of the economically interesting results. The reader is advised that the pXRF results are indicative and do not substitute more reliable methods such as assaying. Furthermore, Due to the potential for sampling bias, the opportunistic readings between the transects are not included in the statistics in the body text of this announcement. |
Other substantive exploration data | Since Greenfields licenced ARC and published its technical report, all substantive exploration data has been published in the GreenX's news releases. |
Further work | The pXRF results are indicative only and are used to verify historical records. Recommended future work includes establishing the distribution of disseminated native copper in the large samples, mineral species in the clays and fines of the Discovery Zone, and total copper content by assay of the Discovery Zone fines. |
JORC Table 1, section 1 | |
Criteria | Arctic Rift Copper project |
Sampling techniques | Samples were collected in the field from proximal scree slopes at Neergaard Dal (their origin being highly certain), and in situ mineralisation at the Discovery Zone. Sampling was done by hand and using a geopick. Large sample volumes were preferentially collected to maximise the representativity. |
Drill techniques | No drilling has ever occurred within the ARC. |
Drill sample recovery | No drilling has ever occurred within the ARC, and recovery data does not exist. |
Logging | No drilling has ever occurred within the ARC, and as such, no logging records exist. |
Sub-sampling techniques and sample preparation | The samples bags were inspected and sorted based on their size fraction, lithology, or state of alteration. The sub-samples were each subject to multiple pXRF analysis. This approach was done to provide an understanding of the grade distribution through various size fractions and rock types. The Company considers this baselining technique as a necessary step ahead of future sampling and assaying. |
Quality of assay data and laboratory tests | A Thermo Scientific Niton portable XRF rental device was used. The manufacturer is reputable and the quality of the device is considered to be good, and the rental provider is reputable. However, while pXRF readings are accurate, they only have small fields of view, which may reduce their reliability on heterogenous mineralisation. XRF technology also relies on there being little air gap between the sensor and the sample, which in a field setting is difficult to achieve consistently. As such, the readings should be treated as indicative rather than absolute. |
Verification of sampling and assaying | Reference standards were brought to ARC, and used to calibrate the pXRF device. No significant drift in precision or reliability was recorded. The lower detection limits for all the elements are far below what is required to trace the fault zones and their mineralisation. While not directly comparable, the historical assay results from the area are consistent with the pXRF readings. |
Location of data points | The data locations and topographic control are based on information the Government publicly discloses. Grids are based on UTM Zones 26 and 27N using the WGS84 Datum. |
Data spacing and distribution | The sampling was opportunistic and erratically spaced. Samples were deliberately collected from what in the field appeared to be unmineralised, partially and well-mineralised material. |
Orientation of data in relation to geological structure | The fault zones (including fissures) control much of the observed mineralisation exposed at the surface. Sampling was done across these faults, and in the case of the Discovery Zone, along strike. |
Sample security | All the reported readings are from in situ locations with GPS locations recorded. Data capture and collation were performed or supervised by geoscientists. The results were uploaded by Greenfields personnel and kept in a secure location in both raw, and collated form. Greenfields personnel had full chain-of-custody of the samples to the reputable, independent courier. No other third parties were involved in the sample handling and Greenfields is unaware of any sample security issues. |
Audits or reviews | No audits or reviews of the pXRF readings was performed. As the Company is not relying on this data in absolute terms, and has historical lab assays for cross-comparison, it does not deem an audit necessary. |
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