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EV RESOURCES LTD Capital/Financing Update 2022

Nov 20, 2022

64887_rns_2022-11-20_99e24ae1-9215-492c-bd18-69edd57050b1.pdf

Capital/Financing Update

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ASX ANNOUNCEMENT

21 November 2022

Confirmed Copper-Silver Zones at Don Enrique Paves Way for Drilling Program

Highlights:

  • Channel sample results have been received from initial sampling in and around a historic exploration drive and crosscut at the Don Enrique Copper Project, located in Jauja Province, Peru.

  • Results indicate continuity of copper-silver-zinc (Cu-Ag-Zn) mineralisation.

  • 28 of the 108 samples demonstrate copper values greater than 0.30% and up to 3.22% Cu.

  • 17 of the samples recorded silver values greater than 30ppm and up to 585ppm Ag.

  • The exploration drive appears to have been driven into a mineralised halo around the primary breccia structures that outcrop at surface.

  • A geophysics programme consisting of 28.8 line km of IP, and 46.8 line km of magnetics, will commence by the end of November 2022.

  • A drilling permit application, which requires community approval under Peruvian regulations, is being finalised for submission.

EV Resources Limited (ASX:EVR) (“ EVR ” or the “Company” ) is pleased to announce that a programme of channel sampling taken from within, and around an old underground exploration drive and crosscut at the Don Enrique copper project in Jauja Province, Peru, has been completed and results received. EVR announced the commencement of exploration work at Don Enrique in an ASX release dated 30[th] August 2022[1] .

The exploration drive and crosscut were developed in the 1960’s by Peruvian company Cerro de Pasco. EVR’s results demonstrate continuity of copper-silver-zinc mineralisation where underground development permitted sampling. It appears that the underground development was driven into the halo of mineralisation alongside one of two primary parallel polymetallic breccia structures.

All underground sample results have been received, while results for surface sampling directly along the strike of the breccia orebody are awaited (Figures 1 and 2). See Table 1 for a full account of the underground sample results.

1 ASX Announcement 30 August 2022 - Exploration Commences at Don Enrique Copper-Silver-Gold Project

evresources.com.au

311-313 Hay St Subiaco, Western Australia 6008 +61 (0) 8 6489 0600 [email protected]

A geophysics programme is due to commence on 21 November 2022. In total, 28.8 line km of Induced Polarisation (IP) testwork and a further 46.8 line km of ground magnetics will be conducted along the breccia structures to test what is interpreted, after mapping and geochemical sampling, to be a potential porphyry structure.

A drilling permit application, which requires community approval under Peruvian regulations, is being finalised for submission.

The fieldwork is supported by the local communities, with whom a constructive relationship has been established. Fertiliser, medical equipment and building materials have been supplied to the community as part of an outreach programme following the agreement reached in September 2022.

The community is supplying casual labour to the exploration campaign. EVR has placed community relations at the centre of its site activities and will continue to build this important relationship.

==> picture [264 x 199] intentionally omitted <==

==> picture [278 x 209] intentionally omitted <==

Figure 1 and 2. Underground and surface channel sampling. Note veining and brecciation in photo 2.

evresources.com.au

311-313 Hay St Subiaco, Western Australia 6008 +61 (0) 8 6489 0600 [email protected]

Underground Sampling Programme

Sampling of underground workings was carried out in the historic adits that were developed for exploratory purposes in the 1960’s. A large number of samples have been collected along the west margin of a quartz breccia vein structure, following the strike (footwall).

This structure exhibits a variety of quartz textures including milky white quartz, sinuous quartz saccharoid veinlets, hyaline quartz, and textures such as dog-tooth, buck, and ribbon quartz. This suggests that several generations of silica deposition occurred. In addition, there are sporadic occurrences of carbonate veins including ankerite and calcite.

Copper mineralisation occurs as a dissemination in hydrothermal breccias, narrower quartz veins, and in a strongly silicified dacitic body (see Figure 4).

The identified minerals are predominantly chalcopyrite, traces of bornite, secondary copper such as malachite and azurite, and the local presence of covellite. Silver (Ag), molybdenum (Mo), zinc (Zn), and lead (Pb) mineralisation occur accompanying the Cu mineralisation, in lower concentrations, in the crosscuts perpendicular to the main structure, and towards a short, poorly developed secondary underground working.

Strong Ag and Zn anomalies are reported in the crosscut sampling (see Figures 5 and 6) where silver sulfosalts, sphalerite, and traces of galena have been identified.

The primary quartz breccia vein structure has a variable width of up to 20 metres. A second subparallel structure with a smaller width is located to the east of the main structure. Both structures present a general strike of NNW-SSE and continue for almost 1 km in length.

Figures 7A and 7B demonstrate an idealised cross section of the mineralised structures and their possible behaviour at depth, including underground exploration work, with Cu anomalies in sampling carried out by EV Resources.

The mineralised structures are located in strongly fractured and deformed volcanic units, predominantly pyroclastic rocks that alternate with lava flows, both of dacitic composition. In the vicinity of the mineralised structures, the volcanic units are affected by strong silicification and quartz-sericite alteration.

Some underground crosscuts were also developed, but based on EVR mapping and sampling, they do not completely cut the breccia vein structure. Figure 4 shows a schematic of the layout of the main structure. Samples with anomalous Cu values occur in the crosscuts but not in the margin or the west wall of the structure, which represents a halo of the main structure.

==> picture [241 x 180] intentionally omitted <==

Figure 3. Surface sampling of a mineralised structure, cutting a continuous channel with a diamond blade.

evresources.com.au

311-313 Hay St Subiaco, Western Australia 6008 +61 (0) 8 6489 0600 [email protected]

==> picture [596 x 635] intentionally omitted <==

Figure 4. Copper anomalies in adit sampling, vein breccia structure.

evresources.com.au

311-313 Hay St Subiaco, Western Australia 6008 +61 (0) 8 6489 0600 [email protected]

==> picture [596 x 642] intentionally omitted <==

Figure 5. Silver anomalies in adit sampling, vein breccia structure.

evresources.com.au

311-313 Hay St Subiaco, Western Australia 6008 +61 (0) 8 6489 0600 [email protected]

==> picture [596 x 639] intentionally omitted <==

Figure 6. Zinc anomalies in adit sampling, vein breccia structure.

evresources.com.au

311-313 Hay St Subiaco, Western Australia 6008 +61 (0) 8 6489 0600 [email protected]

The conceptual model suggests the possibility that the structure is linked to a porphyry-type system at depth. Strongly anomalous values in Mo (Figure 8) are reported at the entrance of the main adit, the northern extension of the vein breccia structure.

The Mo values decrease towards the south in the crosscuts that are towards that orientation. The strong presence of Mo indicates a vector that suggests a possible link to a porphyry-type system at depth, to the north of the structure. This will be tested in the geophysics programme commencing in the week of 21 November 2022.

==> picture [180 x 305] intentionally omitted <==

==> picture [262 x 262] intentionally omitted <==

Figure 7A and 7B. Schematic sections showing the potential behaviour of the breccia vein mineralised structures, including Cu anomalies from sampling in the underground workings.

evresources.com.au

311-313 Hay St Subiaco, Western Australia 6008 +61 (0) 8 6489 0600 [email protected]

==> picture [596 x 587] intentionally omitted <==

Figure 8. Molybdenum anomalies in adit sampling, vein breccia structure

evresources.com.au

311-313 Hay St Subiaco, Western Australia 6008 +61 (0) 8 6489 0600 [email protected]

A conceptual geological model (Figure 9) taken from a Geological Survey of Canada publication suggests a structural interpretation consistent with observations made to date for the Don Enrique Project and shows the spatial location and structural level where the Don Enrique breccia structures could be located, above a porphyry system at depth.

==> picture [455 x 322] intentionally omitted <==

Figure 9. Schematic cross-section of a Cu porphyry system showing mineral zonation and possible relationship to skarn (Cu, Au, Mo, and Ag), manto (Pb, Zn, Ag, and Au), ‘mesothermal’ or ‘intermediate’ precious-metal and base-metal vein (vein1 = Au, Ag; vein2 = Cu, Pb, Zn, Au, Ag) and replacement (breccia/vein = Cu, Ag, and possible Au), and epithermal precious-metal deposits, A = porphyry intrusion; B = volcanic rocks; C = clastic sedimentary rocks; D = carbonate-rich sedimentary rocks; E = Argillic alteration; F = pyritic zone. Taken from M.E. Best, Resources in the Near-Surface Earth, in Treatise on Geophysics (Second Edition), 2015

evresources.com.au

311-313 Hay St Subiaco, Western Australia 6008 +61 (0) 8 6489 0600 [email protected]

Underground Channel Sampling Methodology

Geochemical sampling was conducted by collecting samples from continuous channels in underground workings and surface outcrops. Channels were cut with a manual diamond disc saw and sampled after cleaning the walls. Sample intervals 2 metres long, 5 centimetres wide, and 4 centimetres deep were cut, then retrieved using a chisel, and placed in plastic sample bags with a card bearing a unique sample number, and then secured with a plastic clamp.

Once the sampling process was completed, the sample was marked in the field with phosphorescent spray paint. The samples were transported in company trucks to EVR’s Don Enrique camp and kept protected in a warehouse until they were transported to the laboratory in the city of Lima, maintaining the chain of custody.

A total of 257 samples have been collected to date in two sampling campaigns and submitted for analysis, of which one out of every ten are control samples consisting of both blank and duplicate samples. 108 samples have been analysed with results detailed in Table 1.

Samples were analysed at Certimin Peru, an accredited and internationally certified laboratory. Samples of up to 5kg in weight were prepared under the protocol code GO634, dried at 100ºC, ground to 90% passing through #10ASTM mesh (2mm), quartered and pulverized (250g) to 85% passing through #200 ASTM mesh (75um).

The analysis for gold was performed on aliquots of 30g using the atomic absorption (AA) fire assay method and multi-element analysis code G0153, multi-acid digestion, 35 elements, ICPOES. When detection limits are exceeded, additional analysis is applied. Gold was also tested using Code GOO14 fire test-gravimetry. For copper, analysis code GOO39 and for Ag limits, GOOO2 AAS multi-acid code is applied.

Next Steps

A team of Peruvian based geophysical experts have mobilised to site to commence the programme of 28.8 line km of Induced Polarisation Surveys, and 48.8 line km of Ground Magnetometry on Monday 21 November 2022.

The results of surface sampling along the quartz breccia structures are expected in December 2022, and will be used, along with the underground sample results and the geophysics program, to design the drilling program. The drill permitting application is being finalised for submission during this quarter as necessary requirements have now been met.

ENDS

For further information, please contact:

Luke Martino Adrian Paul Non-Executive Chairman Executive Director Tel: +61 8 6489 0600 Tel: +61 8 6489 0600 E: [email protected] E: [email protected]

This ASX announcement was authorised for release by the Board of EV Resources Limited (EVR).

evresources.com.au

311-313 Hay St Subiaco, Western Australia 6008 +61 (0) 8 6489 0600 [email protected]

Forward Looking Statement

Forward Looking Statements regarding EVR´s plans with respect to its mineral properties and programs are forward-looking statements. There can be no assurance that EVR’s plans for development of its mineral properties will proceed as currently expected. There can also be no assurance that EVR will be able to confirm the presence of additional mineral resources, that any mineralisation will prove to be economic or that a mine will successfully be developed on any of EVR’s mineral properties. The performance of EVR may be influenced by a number of factors which are outside the control of the Company and its Directors, staff, and contractors. These statements include, but are not limited to statements regarding future production, resources or reserves and exploration results. All of such statements are subject to certain risks and uncertainties, many of which are difficult to predict and generally beyond the control of the company, that could cause actual results to differ materially from those expressed in, or implied or projected by, the forward-looking information and statements. These risks and uncertainties include, but are not limited to: (i) those relating to the interpretation of drill results, the geology, grade and continuity of mineral deposits and conclusions of economic evaluations, (ii) risks relating to possible variations in reserves, grade, planned mining dilution and ore loss, or recovery rates and changes in project parameters as plans continue to be refined, (iii) the potential for delays in exploration or development activities or the completion of feasibility studies, (iv) risks related to commodity price and foreign exchange rate fluctuations, (v) risks related to failure to obtain adequate financing on a timely basis and on acceptable terms or delays in obtaining governmental approvals or in the completion of development or construction activities, and (vi) other risks and uncertainties related to the company’s prospects, properties and business strategy. Our audience is cautioned not to place undue reliance on these forward-looking statements that speak only as of the date hereof, and we do not undertake any obligation to revise and disseminate forwardlooking statements to reflect events or circumstances after the date hereof, or to reflect the occurrence of or non-occurrence of any events.

Competent Person’s Statement

The information in this announcement that relates to the Don Enrique Project is based on information compiled by Mr Erik Norum who is a Member of the Australian Institute of Geoscientists. Mr Norum is a full-time employee of EV Resources. Mr Norum has sufficient experience which is relevant to the style of mineralisation and type of deposit under consideration and to the activity which he is undertaking 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”. Mr Norum consents to the inclusion in this announcement of the matters based on information in the form and context in which it appears.

evresources.com.au

311-313 Hay St Subiaco, Western Australia 6008 +61 (0) 8 6489 0600 [email protected]

Table 1. Assay Results from the Don Enrique Sampling Programme

SAMPLE EASTING NORTHING DATUM UTM ZONE LOCATION Auppm Ag ppm Cu % Moppm Pbppm Znppm
14001 459966 8712328 UTMWGS84 18S UNDERGROUND 0.045 94.5 1.18 9 290 264
14002 459966 8712330 UTMWGS84 18S UNDERGROUND 0.016 42.1 0.692 11 140 215
14003 459966 8712332 UTMWGS84 18S UNDERGROUND 0.0025 6.1 0.0352 6 259 112
14004 459965 8712334 UTMWGS84 18S UNDERGROUND 0.0025 12.1 0.0393 17 835 331
14005 459965 8712336 UTMWGS84 18S UNDERGROUND 0.0025 8.9 0.0715 19 870 270
14006 459965 8712338 UTMWGS84 18S UNDERGROUND 0.0025 3.5 0.0862 7 360 251
14007 459965 8712340 UTMWGS84 18S UNDERGROUND 0.0025 11 0.0594 5 783 416
14008 459965 8712342 UTMWGS84 18S UNDERGROUND 0.0025 26 0.2481 18 1453 2181
14009 459964 8712344 UTMWGS84 18S UNDERGROUND 0.0025 3.1 0.0195 6 312 209
14011 459963 8712346 UTMWGS84 18S UNDERGROUND 0.0025 22.3 0.0627 9 183 52.7
14012 459962 8712347 UTMWGS84 18S UNDERGROUND 0.0025 1 0.0304 4 107 63.8
14013 459973 8712328 UTMWGS84 18S UNDERGROUND 0.0025 13.2 0.1766 88 315 608
14014 459973 8712330 UTMWGS84 18S UNDERGROUND 0.007 11.4 0.1765 37 435 403
14015 459974 8712332 UTMWGS84 18S UNDERGROUND 0.035 33.2 0.337 43 629 227
14016 459974 8712334 UTMWGS84 18S UNDERGROUND 0.018 26.4 0.3357 27 607 230
14017 459972 8712336 UTMWGS84 18S UNDERGROUND 0.008 22 0.1915 22 641 365
14018 459972 8712338 UTMWGS84 18S UNDERGROUND 0.011 12.9 0.1167 56 348 1933
14019 459971 8712340 UTMWGS84 18S UNDERGROUND 0.006 13.7 0.1634 207 712 1318
14021 459971 8712342 UTMWGS84 18S UNDERGROUND 0.0025 22.9 0.135 260 1400 2677
14022 459971 8712344 UTMWGS84 18S UNDERGROUND 0.0025 15.3 0.102 178 1424 4548
14023 459971 8712346 UTMWGS84 18S UNDERGROUND 0.0025 30.5 0.1855 516 1123 1840
14024 459971 8712347 UTMWGS84 18S UNDERGROUND 0.0025 6.5 0.062 399 420 221
14025 459998 8712310 UTMWGS84 18S UNDERGROUND 0.0025 3.3 0.0972 6 181 230
14026 459996 8712310 UTMWGS84 18S UNDERGROUND 0.014 6.8 0.1699 14 141 209
14027 459994 8712310 UTMWGS84 18S UNDERGROUND 0.106 50.6 0.5457 9 357 181
14028 459992 8712310 UTMWGS84 18S UNDERGROUND 0.079 585 3.22 84 3551 1579
14029 459990 8712310 UTMWGS84 18S UNDERGROUND 0.0025 17.5 0.2762 32 225 334
14031 459988 8712310 UTMWGS84 18S UNDERGROUND 0.0025 11.8 0.2019 79 305 271
14032 459986 8712310 UTMWGS84 18S UNDERGROUND 0.0025 10 0.258 11 73 122
14033 459984 8712310 UTMWGS84 18S UNDERGROUND 0.007 22.5 0.5698 8 116 204
14034 459996 8712297 UTMWGS84 18S UNDERGROUND 0.0025 5.8 0.2018 4 114 170
14035 459994 8712297 UTMWGS84 18S UNDERGROUND 0.016 6.1 0.3124 15 70 176
14036 459992 8712298 UTMWGS84 18S UNDERGROUND 0.017 7.2 0.242 6 97 198
14037 459990 8712298 UTMWGS84 18S UNDERGROUND 0.021 8.2 0.427 69 158 187
14038 459988 8712299 UTMWGS84 18S UNDERGROUND 0.019 8.9 0.1971 62 244 199
14039 459986 8712299 UTMWGS84 18S UNDERGROUND 0.014 15.4 0.4607 9 79 86.8
14041 459984 8712299 UTMWGS84 18S UNDERGROUND 0.014 8.6 0.2606 4 78 54
14042 459997 8712289 UTMWGS84 18S UNDERGROUND 0.0025 5.1 0.782 4 113 145
14043 459995 8712289 UTMWGS84 18S UNDERGROUND 0.018 19.3 0.2226 4 145 93.5
14044 459993 8712289 UTMWGS84 18S UNDERGROUND 0.025 19.1 0.2594 9 137 241
14045 459991 8712289 UTMWGS84 18S UNDERGROUND 0.036 45.2 0.2822 36 399 268
14046 459989 8712289 UTMWGS84 18S UNDERGROUND 0.0025 7 0.0837 24 397 128
14047 459987 8712289 UTMWGS84 18S UNDERGROUND 0.015 12.4 0.193 92 384 104
14048 459985 8712289 UTMWGS84 18S UNDERGROUND 0.0025 2.7 0.0247 10 140 42.1
14049 459964 8712318 UTMWGS84 18S UNDERGROUND 0.0025 0.3 0.00646 2 40 93.4
14051 459964 8712320 UTMWGS84 18S UNDERGROUND 0.0025 2.7 0.0473 4 420 1246
14052 459964 8712322 UTMWGS84 18S UNDERGROUND 0.0025 60.8 0.8647 5 265 436
14053 459965 8712324 UTMWGS84 18S UNDERGROUND 0.0025 42 0.5728 4 115 361
14054 459965 8712326 UTMWGS84 18S UNDERGROUND 0.008 29.3 0.3059 8 152 389
14055 459997 8712266 UTMWGS84 18S UNDERGROUND 0.0025 6.3 0.0708 5 549 2922
14056 459995 8712267 UTMWGS84 18S UNDERGROUND 0.021 51.5 0.3469 3 738 325
14057 459993 8712268 UTMWGS84 18S UNDERGROUND 0.18 367 2.81 3 1115 533
14058 459991 8712269 UTMWGS84 18S UNDERGROUND 0.035 78.2 0.4618 21 1744 1275
14059 459989 8712270 UTMWGS84 18S UNDERGROUND 0.012 55.1 0.3593 23 1748 1264
14060 459987 8712271 UTMWGS84 18S UNDERGROUND 0.015 26.2 0.2737 4 499 149
14062 459985 8712272 UTMWGS84 18S UNDERGROUND 0.012 34.2 0.3717 35 542 157
14063 459984 8712273 UTMWGS84 18S UNDERGROUND 0.038 36.9 0.2858 4 651 356
14064 459982 8712273 UTMWGS84 18S UNDERGROUND 0.008 26.4 0.1849 24 7240 1471
14065 459971 8712327 UTMWGS84 18S UNDERGROUND 0.007 17.4 0.3109 94 726 1439
14066 459971 8712325 UTMWGS84 18S UNDERGROUND 0.0025 11.1 0.1484 115 709 3154
14067 459972 8712322 UTMWGS84 18S UNDERGROUND 0.006 19.5 0.2937 14 605 446
14068 459972 8712320 UTMWGS84 18S UNDERGROUND 0.0025 5.2 0.0801 33 296 1488
14069 459974 8712319 UTMWGS84 18S UNDERGROUND 0.0025 10.5 0.163 369 466 2048
14071 459975 8712318 UTMWGS84 18S UNDERGROUND 0.0025 0.8 0.00722 6 38 156
14072 459977 8712316 UTMWGS84 18S UNDERGROUND 0.0025 0.3 0.00578 6 46 86.5
14073 459978 8712315 UTMWGS84 18S UNDERGROUND 0.0025 1 0.0153 4 53 111
14074 459980 8712313 UTMWGS84 18S UNDERGROUND 0.0025 1.7 0.026 4 79 148
14075 459981 8712312 UTMWGS84 18S UNDERGROUND 0.0025 2.2 0.0676 26 103 335
14076 459981 8712310 UTMWGS84 18S UNDERGROUND 0.0025 5.7 0.1655 28 144 179
14077 459981 8712308 UTMWGS84 18S UNDERGROUND 0.0025 12.9 0.381 14 194 175
14078 459981 8712306 UTMWGS84 18S UNDERGROUND 0.0025 1.1 0.0409 6 66 115
14079 459981 8712304 UTMWGS84 18S UNDERGROUND 0.0025 0.8 0.0316 8 53 94.7
14081 459981 8712302 UTMWGS84 18S UNDERGROUND 0.0025 1.2 0.0367 3 77 209
14082 459980 8712300 UTMWGS84 18S UNDERGROUND 0.0025 0.8 0.0101 2 105 323
14083 459980 8712298 UTMWGS84 18S UNDERGROUND 0.0025 1.9 0.0581 3 182 142
14084 459980 8712296 UTMWGS84 18S UNDERGROUND 0.0025 3.2 0.1001 5 329 273
14085 459980 8712294 UTMWGS84 18S UNDERGROUND 0.025 55.4 1.31 8 666 243
14086 459980 8712294 UTMWGS84 18S UNDERGROUND 0.0025 3 0.0816 4 220 123
14087 459980 8712292 UTMWGS84 18S UNDERGROUND 0.011 17.6 0.3734 7 1506 439
14088 459980 8712292 UTMWGS84 18S UNDERGROUND 0.0025 1.6 0.0346 4 199 107
14089 459980 8712290 UTMWGS84 18S UNDERGROUND 0.0025 0.8 0.017 7 84 171
14090 459980 8712288 UTMWGS84 18S UNDERGROUND 0.0025 0.6 0.0107 5 41 103
14092 459981 8712286 UTMWGS84 18S UNDERGROUND 0.0025 1.9 0.00851 5 288 105
14093 459981 8712284 UTMWGS84 18S UNDERGROUND 0.0025 2.1 0.0172 4 1174 687
14094 459981 8712282 UTMWGS84 18S UNDERGROUND 0.0025 1.4 0.0169 4 539 547
14095 459980 8712280 UTMWGS84 18S UNDERGROUND 0.008 28.4 0.4274 21 716 1483
14096 459980 8712280 UTMWGS84 18S UNDERGROUND 0.0025 1.4 0.00964 3 191 128
14097 459980 8712279 UTMWGS84 18S UNDERGROUND 0.019 59.4 0.8675 21 461 469
14098 459980 8712279 UTMWGS84 18S UNDERGROUND 0.0025 1.9 0.0165 4 83 36.5
14099 459979 8712277 UTMWGS84 18S UNDERGROUND 0.0025 10.8 0.0222 22 411 82.1
14101 459979 8712275 UTMWGS84 18S UNDERGROUND 0.0025 1.5 0.00977 4 56 476
14102 459979 8712273 UTMWGS84 18S UNDERGROUND 0.0025 1.5 0.00634 3 95 77.4
14103 459985 8712258 UTMWGS84 18S UNDERGROUND 0.0025 0.1 0.0041 2 79 253
14104 459984 8712260 UTMWGS84 18S UNDERGROUND 0.0025 1.7 0.0396 12 473 186
14105 459983 8712261 UTMWGS84 18S UNDERGROUND 0.008 7.1 0.1347 102 1521 265
14106 459982 8712263 UTMWGS84 18S UNDERGROUND 0.0025 8.8 0.0789 24 531 147
14107 459981 8712265 UTMWGS84 18S UNDERGROUND 0.0025 4.1 0.0379 5 234 90.9
14108 459980 8712267 UTMWGS84 18S UNDERGROUND 0.01 41.1 0.1078 31 607 78.1
13501 459982.4 8712351 UTMWGS84 18S SURFACE 0.0025 2.8 0.0475 17 128 237
13502 459981.6 8712349.2 UTMWGS84 18S SURFACE 0.0025 12.2 0.1985 9 123 160
13503 459980.4 8712347.6 UTMWGS84 18S SURFACE 0.026 134 0.5477 44 1248 419
13504 459977.4 8712346.2 UTMWGS84 18S SURFACE 0.018 46.4 0.3055 57 712 1083
13505 459976.4 8712342.8 UTMWGS84 18S SURFACE 0.008 17 0.1096 13 373 157
13506 459975 8712346.2 UTMWGS84 18S SURFACE 0.0025 12 0.0808 57 192 191
13507 459973.4 8712346.2 UTMWGS84 18S SURFACE 0.011 15.9 0.1489 14 411 129
13508 459968 8712350.6 UTMWGS84 18S SURFACE 0.0025 4.9 0.0367 29 112 49.7
13509 459966.8 8712349.6 UTMWGS84 18S SURFACE 0.006 24.1 0.3792 20 423 105
13511 459923 8712367 UTMWGS84 18S SURFACE 0.0025 0.8 0.0122 22 104 58.5
* ‘x’ = below limit of detection

evresources.com.au

311-313 Hay St Subiaco, Western Australia 6008 +61 (0) 8 6489 0600 [email protected]

JORC Code, 2012 Edition – Table 1 report

Section 1 Sampling Techniques and Data

(Criteria in this section apply to all succeeding sections.)

Criteria 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
30 g 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 (e.g. submarine
nodules) may warrant disclosure of detailed information.
Continuous channels in underground workings and surface outcrops were cut with a
manual diamond disc cutter. Samples were 2 meters long, 5 centimetres wide, and 4
centimetres deep.
No instruments were used to determine mineralisation.
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). _
No drilling reported.

evresources.com.au

311-313 Hay St Subiaco, Western Australia 6008 +61 (0) 8 6489 0600

[email protected]

Criteria Explanation Commentary
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 topreferential loss/gain of fine/coarse material.
No drilling reported.
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.
No drilling reported.
Geology of rock chip channel samples was recorded. Geological records have primarily
been quantitative.
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.
At the laboratory, samples were dried crushed and pulverised to 90% passing through
#10ASTM mesh (2mm). The sample was then quartered and pulverized (250g) to 85%
passing through #200 ASTM mesh (75um). This is considered to appropriately
homogenise the sample to allow subsampling for the various assay techniques.
One out of every ten samples are control samples consisting of both blank and
duplicate samples.
Sample sizes are industry standard and considered appropriate.
Quality of assay
data and laboratory
tests

The nature, quality and appropriateness of the assaying
and laboratory procedures used and whether the
technique is consideredpartial or total.
Analysis for gold was performed on aliquots of 30 g using the atomic absorption (AA)
fire assaymethod and Multi element analysis code G0153, multi-acid digestion, 35

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Criteria Explanation Commentary

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 (e.g.
standards, blanks, duplicates, external laboratory checks)
and whether acceptable levels of accuracy (i.e. lack of bias)
and precision have been established.
elements, ICP-OES. When detection limits are exceeded, additional analysis is
applied. Gold was also tested using Code GOO14 fire test-gravimetry. For Copper,
analysis code GOO39 and for Ag limits, GOOO2 AAS multi-acid code is applied.
Analyses are considered partial.
One out of every ten samples are control samples consisting of both blank and
duplicate samples.
Sample sizes are industry standard and considered appropriate.
LaboratoryQAQC was undertaken.
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.
No drilling reported.
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.
Rock Chip channel location were surveyed using handheld GPS. Garmin GPSMAP 64s
The grid used was UTM Zone 18, datum WGS84
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.
Not Applicable as no JORC-2014 resource estimate has been completed.
Sampling was of a reconnaissance nature.
No compositing of samples or results was applied.
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.
No drilling reported.

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Criteria Explanation Commentary

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.
Sample security
The measures taken to ensure sample security.
Sample chain of custody was managed by the employees of EV resources. All samples
were bagged and tied in numbered plastic bags, grouped into larger tied polyweave
bags in the field. Samples collected in the field were transported by geological staff
to the Don Enrique site base, then directlyto the lab.
Audits or reviews
The results of any audits or reviews of sampling techniques
and data.
No audits or reviews were deemed necessary as this work is purely qualitative assaying
for first-pass explorationpurposes.

Section 2 Reporting of Exploration Results

(Criteria listed in the preceding section also apply to this section.)

Criteria 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.
Don Enrique Project is made up of 4 mining rights: Cocoa Beach, Don Enrique 85,
Chaupiloma 2008, and Chaupiloma 2007. It is under a purchase option agreement with a
local company that is the holder of the 4 mining concessions that cover a total of 1802
hectares.
There are no archaeological remains and it is not included in any national park which
prevents its normal development of mining exploration. It is located within two
communities, Quero and Yauli.
Exploration done by
otherparties

Acknowledgment and appraisal of exploration by other
parties.
Geology
Deposit type, geological setting and style of
mineralisation.
Don Enrique corresponds to a Cu-Ag-Pb-Zn intermediate sulfidation polymetallic
epithermal deposit with some Au credits. It is a breccia vein structure ranging from 5 to 20
meters wide and 1200 meters long, occurring irregularly on strike. It is housed in volcanic
rocks, pyroclastic units that alternate with lava flows of dacitic composition. Development
of hydrothermal breccias cuttingthrough the breccia vein structure. Mineralization occurs

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Criteria Explanation Commentary
as dissemination of Cu sulfides, secondary Cu and Cu-quartz veinlets emplaced in the
breccia vein structure.
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.
No drilling was undertaken.
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 drilling was undertaken.
No averaging or aggregating of rock chip results was undertaken.
Individual results have been reported.
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.
No drilling was undertaken.
No geometry or width is reported with rock samples.

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Criteria Explanation Commentary

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’). _
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.
No drilling was undertaken.
A sample location plan is included as Figures 1 to 3 and Figure 5.
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 results have been reported.
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.
All meaningful & material exploration data has been reported.
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.
Exploration at Don Enrique is at an early stage. Drill targets will be delineated once
imminent geophysical surveys have been completed and the data assessed.

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