Solis Minerals Provides Updated on Exploration Activities at the Cinto Project in Peru

Copper Porphyry Mineralisation Confirmed at Cinto 0.88% Cu over 23.4m

HIGHLIGHTS

• Extensive copper porphyry mineralisation identified in rock and channel sampling at Cinto Project, Peru.

Highlights include:

• 23.4m @ 0.88% Cu (Channel 1)

• 16.83m @ 0.52% Cu (Channel 6)

• Cinto is located 15km SE of one of Peru’s major copper mines, Toquepala (2,105mt @ 0.47% Cu resource- 200ktpa Cu production)¹

• Scope for scale with potential porphyry style copper mineralisation over 1.75 square kilometres based on strong correlation of rock geochemistry and a large magnetic low geophysical anomaly, indicating widespread hydrothermal alteration.

• Induced-Polarisation (IP) survey planning now underway following successful geochemical results.

• Drill target definition underway and permitting initiated for drilling in second half of 2025.

Perth, Western Australia–(Newsfile Corp. – February 11, 2025) – Latin American focused copper-gold explorer, Solis Minerals Limited (ASX: SLM) (TSXV: SLMN) (OTCQB: SLMFF) (“Solis” or the “Company”) is pleased to announce an update on exploration activities at the Cinto Project in Peru.

Summary

The copper mineralisation at Cinto is predominantly seen in breccias, the major mineralisation host at the Toquepala Copper Mine, 15km northwest of Cinto. Geological similarities are evident between mineralisation styles at Cinto and Toquepala. Cinto is situated on the major Incapuquio Fault System which favoured the emplacement of intrusions related to large-scale porphyry copper deposits of Toquepala, Quellaveco, and Cuajone (Figure 1). Toquepala is one of Peru’s major copper producers (200ktpa).

¹ Total Mineral Reserves for third party mines sourced from Southern Copper 10K Report 2023, lodged with SEC 31 December 2023 (Cuajone & Toquepala) and Anglo American (LSE:AAL) Annual Report 2023

Executive Director, Mike Parker, commented:

“The Cinto Project continues to deliver excellent results and we have considerably expanded our porphyry copper mineralisation footprint. Equally exciting is that we are observing styles of copper mineralisation that resemble the main mineralisation styles of the massive Toquepala mine (196,600tpa copper) only 15km to the northwest. Our drone magnetometry geophysics correlates well with mineralisation and indicates potential for scale as well as new areas to follow-up. As a stand-alone project, Cinto is shaping up well as a significant mineralised copper porphyry target. When combined with our advanced targets and planned drilling at our Coastal Belt projects, our copper portfolio is truly outstanding.

This year will be a year of building on all the hard ground work of identifying our drill targets in 2024. We will start drilling at two of our projects, Chancho al Palo and Ilo Este, later this quarter depending on permits, while the Cinto Project will be advanced to drill in second half of 2025″.

Cinto Project

The Cinto Project consists of eight tenements totalling 3,169Ha in the highly prospective Cenozoic Porphyry Belt of southern Peru, located some 15km to the southeast of the world class Toquepala Copper Mine (Figure 1). Cinto is geologically distinct from the rest of Solis’ tenements which are situated in the older Jurassic-Cretaceous Coastal Belt of Peru (Figure 3).

Figure 1: Cinto tenements, Incapuquio Fault System, and geology.

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Figure 2: Cinto Project Channel 7, sample 18369, taken across mineralisation in brecciated andesitic tuff exposed by gully erosion. Sample length 1.1m. Assay results: Au 0.535 g/t, Ag 25 g/t, Cu 8.7%, Mo 1 ppm, Pb 283 ppm, Zn 873 ppm.

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Figure 3: Solis’ tenements in the Coastal and Cenozoic (Paleocene-Eocene) Belts with existing deposits and regional geology shown. Note new permit applications made north of Cinto in January 2025.

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Results of rock and channel geochemistry sampling programs carried out at Cinto in the second half of 2024 have yielded highly encouraging results that confirm porphyry mineralisation over a broad area. Rock samples were collected from outcropping rocks of interest or on a sampling grid, whilst Channel Samples were continuous samples taken across zones of outcropping mineralisation, usually related to old workings or eroded gullies.

A site with historical workings previously rock sampled during reconnaissance surveys by Solis and reported in July 20242, has now returned 0.88% Cu over 23.40m in Channel 1. Approximately 500m to the east of the reconnaissance site, Channel 6 returned 0.52% Cu over 16.83m. Values of 5.80% Cu over 2.20m are also reported in an area 630m east of the reconnaissance site in Channel 7, whilst a high-grade narrow (20cm) vein and one metre wallrock grading 10.32% lead and 2.31% zinc was discovered in Channel 5 which is 2.5km to the east of the reconnaissance site at (coordinates East 337396 and North 8079489, Figure 6, Tables 1 & 3). Following these initial geochemical and mapping surveys, the Company is planning the layout of an IP survey in various zones to define drill targets.

A strong correlation is identified between copper mineralisation defined in the geochemical program and previously reported magnetic low geophysical anomalies (Figures 4 & 7). In the northeast of the licence, all channel samples and the majority of copper-anomalous rock samples fall within a magnetic low of dimensions 3km x 0.75km with the low core having a surface area of 1.75km2 creating scope for scale. This magnetic low anomaly is interpreted as being caused by magnetite destruction, a common occurrence in porphyry deposits where late-stage mineralising fluids react with magnetic minerals in a host rock, altering them to non- magnetic mineral species. Two further magnetic low anomalies are recognised locally – one with dimensions of 1km x 0.3km to the west of the low described above; and a further zone of 3.5 x 1.0km to the southwest (X and Y on Figure 7). Both areas are yet to be sampled, and the latter has coincident alteration mapped from WorldView-3 satellite studies previously reported2. Based on results to date, both areas are considered to be highly prospective for further porphyry copper mineralisation.

Previous Exploration at Cinto

Prior to Solis acquiring the Cinto tenements, limited systematic exploration had been completed and there are no records of previous drill programs. Solis commenced exploration with a WorldView-3 remote sensing survey, followed up by geological mapping. In 2023 and 2024, reconnaissance rock sampling led to the identification of an area of in-situ copper oxide mineralisation in old workings in the northeast of the property. Several samples returned assays in excess of 1% Cu (highest 7.14% Cu) in a circular area roughly 100m in diameter (Figure 4). In late 2024, Solis completed a drone magnetometry survey that identified areas of low magnetic response coincident and extending beyond the reconnaissance mineralisation3. Previous exploration results are summarised in Figure 4.

² Solis ASX release 9 July 2024, High Grade Copper Samples Identified at Cinto
³ Solis ASX release 15 October 2024, Solis Completes Magnetometry Survey at Cinto

Figure 4: Previous exploration at Cinto: Total Field magnetic data (high magnetic response in red, low response in blue) overlaid by WorldView-3 alteration suites and geology/structure. “Cu” marks zone of high grade copper oxide samples from old workings, the original reconnaissance site sampled 1H 2024.

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Cinto Structural Setting

Cinto sits astride or just south of the regional transcurrent Incapuquio Fault System (Figures 1 & 4). The fault’s corridor of influence includes en echelon faults, and subparallel fault structures. In the Cinto area, the fault corridor has an approximate width of 2.5km across its predominant NW-SE strike direction. This fault system is believed to have influenced the emplacement of Late Cretaceous to Early Palaeogene (Cenozoic) granodioritic, dioritic, and monzonitic intrusions as well as related volcanic rocks of the Toquepala Group4. The large- scale copper porphyry deposits of Cuajone, Quellaveco, and Toquepala were formed during this intrusive phase (Figure 3) and are associated with, or emplaced within, volcanics of the Toquepala Group.

Cinto Mineralisation Style

In the reconnaissance area (Channel Samples 1-4, Figure 6), the mineralisation is localised in brecciated altered andesitic tuffs of the Toquepala Group. Quartz veining is seen forming the matrix of grossly brecciated and phylically altered units (Figure 5). Copper oxides are visible in the quartz veining and replacing tuffs in patches. Millimetric size textures on the veins and wallrocks are characteristic of intrusive hydrothermal breccias.

⁴ Structural Characteristics of the Incapuquio fault system, southern Peru, J. Jacay, T. Sempere et al, 2002

Figure 5: Channel 4 (viewed from north) sampled across brecciated and altered andesitic tuff outcrop exposed by old workings. Width of photo field of view is approximately 7m. Assay results returned over 0.00-5.50m (4.50m linear) are Au 0.011 ppm, Ag 3 ppm, Cu 1.03%, Mo 1 ppm, Pb 128 ppm, Zn 212 ppm.

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In the areas of Channel Samples 6-10 (Figure 6), the mineralisation occurs in intrusive hydrothermal breccias that have impacted andesitic tuffs of the Toquepala Group (Figure 2). Brecciation consists of quartz veining that separates and cross-cuts angular tuff clasts. Alteration includes abundant phyllic alteration and silicification. Copper oxide minerals occur in the quartz veins and also in patches and segregations in the clasts.

The above occurrences both resemble various phases of mineralisation at the Toquepala Copper Mine, some 15km northwest of Cinto, where intrusive hydrothermal breccias are a significant mineralisation host. The geochemistry reveals low to sporadic gold values which also resembles Toquepala. Generally low molybdenum values can be attributed to oxidation.

An outcrop of a mineralised quartz vein (20cm wide) occurs in granodiorites in the east of the property (Channel 5, Figure 6) and including 1m of granodiorite wallrock grades 10.32% lead and 2.31% zinc. Channel 5 is 2.5km to the east of the reconnaissance site at coordinates East 337396 and North 8079489. This occurrence is considered as a lateral expression to the copper-dominated mineralisation further west.

Cinto Geochemical Sampling 2024

During 2H 2024, 485 rock samples were collected (Tables 1-4). Of these, 333 were outcrop rock samples and 152 were channel samples from 10 separate channels. Channel sampling was carried out in areas of good to continuous outcrop, usually facilitated by the presence of old (>50 years) small scale surface workings – Channels 1,2,3,4,6,9,10 – or in areas of gully erosion. The 2H 2024 program complements the 45 rock samples taken in late 2023/1H 20242 and brings the total rock sampling inventory at Cinto to 530 samples.

The channels sampled are indicated in zones on the locality map, Figure 6 and results summarised in Table 1 with details in Table 3.

Figure 6: Cinto locality map of channel sampling areas underlain by total field drone magnetometry. Note that the channel sampling is located in zones of low magnetic response (blue-green colours) indicating hydrothermal alteration. The magnetometry is a valuable guide for exploration at Cinto. Channels 1-4 are located over the original reconnaissance site, reported in July 2024.

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A summary of the channel sampling assay results is presented below in Table 1.

Table 1: Summary of channel sample geochemical assay results from Cinto Project. Zones highlighted in bold are >0.5% Cu. True length is calculated taking into account the linearity of the sampling line. Sampling was done predominantly at a high angle to outcrop strike within the constraints of shallow channel sampling.

For location coordinates of channel samples and all assays, refer Table 3, Appendix 1.

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Additionally, 333 rock outcrop samples were analysed in an area of approximately 6 x 2km in the east of the permits. The results from these samples (Table 2 Table 4, Appendix 1) show a correlation of copper mineralisation with alteration (low magnetic response areas) around structures (Figure 7). Table 2 shows the highest Cu assays returned in rocks (does not include channel samples) and their geological context.

Table 2: Cinto rock samples geochemical assays reporting >0.5% Cu (17 out of 333 samples). Those in bold are within porphyry-style assemblages. Altered granodiorites are considered marginal to potential porphyry system. Note veins in granodiorite with high base metal values in east, close to Channel 5.

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Figure 7: Cu anomalies from rock sample assays centred around structures with hydrothermal alteration. “X” and “Y” represent prospective areas of low magnetic response yet to be evaluated.

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Results of the geochemical surveys

Following up on the initial rock geochemical sampling campaign of the reconnaissance site, the channel sampling and rock sampling geochemical results have:

• confirmed the presence of porphyry style copper mineralisation in favourable structural locations with analogous characteristics to the nearby Toquepala porphyry

• expanded the area of interest at Cinto with two newly discovered Cu-mineralised zones (Channels 6 & 7-10) 500m and 630m east of the reconnaissance site (Channels 1-4)

• demonstrated a strong spatial correlation of copper mineralisation with the magnetic low geophysical anomaly that indicates a zone of hydrothermal alteration. Several such areas, particularly to the west of the project, have yet to be evaluated, indicating a potential for further large-scale mineralised systems at Cinto

• demonstrated the potential for associated polymetallic mineralisation (Pb, Zn, Ag) around the copper-dominated area with the discovery of highly mineralised, narrow structures approximately 2.5km east of the original site (Channel 5) and adjacent rock samples.

Next Steps for Cinto

Based on the geochemistry results, Induced-Polarisation (IP) programs are being planned to define drill targets. Drill permitting, including archaeological surveys, will commence with a target of drilling in the second half of 2025.

Solis will continue to investigate the potential of Cinto by testing the as yet unexplored low magnetic anomalies through a combination of mapping and rock geochemistry. Further areas for IP follow-up and drill target definition are expected to become apparent once all the tenement is explored.

5. Drilling Schedule

* Timeline dependent upon obtaining requisite permits

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ENDS

 

Neither the TSX Venture Exchange nor its Regulation Service Provider (as the term is defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy of accuracy of this news release.

About Solis Minerals Limited

Solis Minerals is an emerging exploration company, focused on unlocking the potential of its South American copper portfolio. The Company is building a significant copper portfolio around its core tenements of Ilo Este and Ilo Norte and elsewhere in the Coastal Belt of Peru and currently holds 81 exploration concessions for a total of 69,200Ha (46 concessions granted with 35 applications in process).

The Company is led by a highly-credentialled and proven team with excellent experience across the mining lifecycle in South America. Solis is actively considering a range of copper opportunities. South America is a key player in the global export market for copper and Solis, under its leadership team, is strategically positioned to capitalise on growth the opportunities within this mineral-rich region.

Forward-Looking Statements

This news release contains certain forward-looking statements that relate to future events or performance and reflect management’s current expectations and assumptions. Such forward- looking statements reflect management’s current beliefs and are based on assumptions made and information currently available to the Company. Readers are cautioned that these forward- looking statements are neither promises nor guarantees and are subject to risks and uncertainties that may cause future results to differ materially from those expected, including, but not limited to, market conditions, availability of financing, actual results of the Company’s exploration and other activities, environmental risks, future metal prices, operating risks, accidents, labour issues, delays in obtaining governmental approvals and permits, and other risks in the mining industry. All the forward-looking statements made in this news release are qualified by these cautionary statements and those in our continuous disclosure filings available on SEDAR+ at www.sedarplus.ca. These forward-looking statements are made as of the date hereof, and the Company does not assume any obligation to update or revise them to reflect new events or circumstances save as required by applicable law.

Qualified Person Statement

The technical information in this news release was reviewed by Michael Parker, a Fellow of the Australian institute of Mining and Metallurgy (AusIMM), a qualified person as defined by National Instrument 43-101 (NI 43-101). Michael Parker is Executive Director of the Company.

Competent Person Statement

The information in this ASX release concerning Geological Information and Exploration Results is based on and fairly represents information compiled by Mr Michael Parker, a Competent Person who is a Fellow of the Australasian Institute of Mining and Metallurgy. Mr Parker is Executive Director of Solis Minerals Ltd. and has sufficient experience which is relevant to the style of mineralisation and types of deposit under consideration and to the exploration activities undertaken to qualify as a Competent Person as defined in the 2012 Edition of the “Australian Code for Reporting of Mineral Resources and Ore Reserves”. Mr Parker consents to the inclusion in this report of the matters based on information in the form and context in which it appears. Mr Parker has provided his prior written consent regarding the form and context in which the Geological Information and Exploration Results and supporting information are presented in this Announcement.

APPENDIX 1

Table 3 Cinto Channel Sample Geochemical Assay Results

Sample No.	E Coord	N Coord	Elev.	Chan No.	Notes	Int. From m	Int. To m	Linear Distance m	Corrected Distance m	Au ppm	Ag ppm	Cu %	Mo ppm	Pb ppm	Zn ppm
18095	335127	8079472	2360	CH1	Start Channel Sample	0.00	2.00	2.00	1.70	0.003	1.30	0.06	1	45	444
18096	335127	8079474	2360	CH1		2.00	4.00	2.00	1.70	0.003	4.00	0.03	1	50	270
18097	335127	8079475	2360	CH1		4.00	5.00	1.00	0.85	0.003	7.90	1.55	1	281	797
18098	335126	8079476	2360	CH1		5.00	6.00	1.00	0.85	0.007	6.40	0.16	1	344	348
18099	335126	8079477	2360	CH1		6.00	7.00	1.00	0.85	0.003	4.80	0.11	1	484	492
18100	335125	8079478	2360	CH1		7.00	8.00	1.00	0.85	0.003	4.00	0.09	1	437	250
18102	335125	8079478	2360	CH1		8.00	9.00	1.00	0.85	0.003	3.20	0.07	1	442	416
18103	335123	8079479	2360	CH1		9.00	11.00	2.00	1.70	0.003	0.70	0.03	1	149	215
18104	335121	8079479	2360	CH1		11.00	13.00	2.00	1.70	0.003	0.70	0.01	1	104	205
18105	335119	8079480	2360	CH1		13.00	15.00	2.00	1.70	0.003	0.90	0.01	1	142	283
18106	335117	8079480	2360	CH1		15.00	17.00	2.00	1.70	0.003	0.90	0.02	1	219	305
18107	335116	8079480	2360	CH1		17.00	18.00	1.00	0.85	0.003	0.80	0.02	1	293	308
18108	335115	8079479	2360	CH1		18.00	19.00	1.00	0.85	0.003	0.80	0.02	1	232	346
18109	335114	8079479	2360	CH1		19.00	20.00	1.00	0.85	0.003	1.00	0.02	1	97	270
18110	335113	8079479	2360	CH1		20.00	21.00	1.00	0.85	0.003	1.70	0.20	1	212	260
18111	335112	8079479	2360	CH1		21.00	22.00	1.00	0.85	0.003	3.00	0.23	1	65	275
18112	335111	8079480	2360	CH1		22.00	23.00	1.00	0.85	0.036	5.50	1.86	1	72	225
18113	335110	8079479	2360	CH1		23.00	24.00	1.00	0.85	0.011	3.40	0.88	1	39	302
18114	335109	8079479	2360	CH1		24.00	25.00	1.00	0.85	0.009	3.20	0.43	1	113	306
18115	335108	8079479	2360	CH1		25.00	26.00	1.00	0.85	0.017	4.40	0.84	1	84	541
18116	335107	8079479	2360	CH1		26.00	27.00	1.00	0.85	0.007	3.00	0.66	1	121	381
18117	335106	8079479	2360	CH1		27.00	28.00	1.00	0.85	0.003	2.00	0.06	1	311	276
18118	335105	8079479	2360	CH1		28.00	29.00	1.00	0.85	0.003	3.80	0.06	1	108	219
18119	335105	8079479	2360	CH1		29.00	30.00	1.00	0.85	0.003	2.00	0.03	1	71	179
18121	335104	8079478	2360	CH1		30.00	31.00	1.00	0.85	0.003	2.00	0.19	1	150	237
18122	335103	8079479	2360	CH1		31.00	32.00	1.00	0.85	0.037	5.50	4.33	1	524	331
18123	335102	8079479	2360	CH1		32.00	33.00	1.00	0.85	0.032	3.60	1.40	1	65	199
18124	335101	8079480	2360	CH1		33.00	34.00	1.00	0.85	0.061	6.40	2.04	1	59	248
18125	335100	8079480	2360	CH1		34.00	35.00	1.00	0.85	0.153	5.00	3.91	1	72	305
18126	335099	8079480	2360	CH1		35.00	36.00	1.00	0.85	0.006	2.20	0.27	1	75	246
18127	335098	8079481	2360	CH1		36.00	37.00	1.00	0.85	0.003	1.30	0.07	1	57	205
18128	335097	8079481	2360	CH1		37.00	38.00	1.00	0.85	0.003	1.80	0.05	1	46	190
18129	335096	8079482	2360	CH1		38.00	39.00	1.00	0.85	0.008	1.70	0.05	1	49	224
18130	335095	8079482	2360	CH1		39.00	40.00	1.00	0.85	0.078	6.20	2.77	1	29	579
18131	335095	8079483	2360	CH1		40.00	41.00	1.00	0.85	0.009	2.30	0.02	1	43	165
18132	335094	8079484	2360	CH1		41.00	42.00	1.00	0.85	0.007	2.30	0.03	1	99	149
18133	335093	8079484	2360	CH1		42.00	43.00	1.00	0.85	0.101	3.30	1.55	1	51	117
18134	335092	8079484	2360	CH1		43.00	44.00	1.00	0.85	0.006	4.10	0.06	1	142	233
18135	335091	8079484	2360	CH1		44.00	45.00	1.00	0.85	0.035	4.70	0.97	1	46	183
18136	335090	8079485	2360	CH1		45.00	45.50	0.50	0.43	0.003	0.80	0.07	1	31	210
18137	335090	8079485	2360	CH1		45.50	46.50	1.00	0.85	0.012	2.70	0.11	1	26	82
18138	335089	8079486	2360	CH1		46.50	47.50	1.00	0.85	0.027	12.30	1.06	1	15	100
18139	335088	8079486	2360	CH1		47.50	48.50	1.00	0.85	0.003	1.40	0.03	1	36	177
18140	335087	8079486	2360	CH1		48.50	49.50	1.00	0.85	0.003	0.90	0.01	1	66	240
18142	335086	8079487	2360	CH1		49.50	50.50	1.00	0.85	0.003	1.10	0.01	1	194	464
18143	335085	8079487	2360	CH1		50.50	51.50	1.00	0.85	0.003	0.80	0.01	1	690	443
18144	335084	8079487	2360	CH1		51.50	52.50	1.00	0.85	0.003	1.10	0.03	1	2160	739
18145	335083	8079488	2360	CH1		52.50	53.50	1.00	0.85	0.003	1.00	0.01	2	1675	980
18146	335083	8079488	2360	CH1		53.50	54.50	1.00	0.85	0.003	1.80	0.02	2	2090	773
18147	335081	8079489	2360	CH1		54.50	56.50	2.00	1.70	0.003	1.10	0.01	1	1045	375
18148	335080	8079490	2360	CH1		56.50	58.50	2.00	1.70	0.003	0.80	0.01	1	671	356
18149	335078	8079491	2360	CH1		58.50	60.50	2.00	1.70	0.003	0.80	0.01	2	217	250
18150	335076	8079492	2360	CH1		60.50	62.50	2.00	1.70	0.003	0.60	0.01	1	99	287
18151	335075	8079493	2360	CH1		62.50	64.50	2.00	1.70	0.003	0.60	0.01	1	95	265
18152	335073	8079494	2360	CH1		64.50	66.50	2.00	1.70	0.003	0.50	0.00	1	58	231
18153	335072	8079495	2360	CH1		66.50	68.50	2.00	1.70	0.003	0.50	0.01	1	40	180
18154	335071	8079497	2360	CH1		68.50	69.50	1.00	0.85	0.005	0.90	0.04	1	162	235
18155	335070	8079498	2360	CH1		69.50	70.50	1.00	0.85	0.003	0.25	0.02	1	268	238
18156	335070	8079499	2360	CH1		70.50	72.50	2.00	1.70	0.003	0.25	0.00	1	44	192
18157	335069	8079501	2360	CH1		72.50	74.50	2.00	1.70	0.003	0.25	0.01	1	47	173
18158	335068	8079502	2360	CH1		74.50	76.50	2.00	1.70	0.003	0.70	0.02	1	87	213
18159	335067	8079504	2360	CH1		76.50	78.50	2.00	1.70	0.003	0.70	0.03	1	534	286
18161	335067	8079506	2360	CH1		78.50	80.50	2.00	1.70	0.003	0.80	0.03	1	436	356
18162	335066	8079508	2360	CH1		80.50	82.50	2.00	1.70	0.003	0.80	0.02	1	211	262
18163	335066	8079510	2360	CH1		82.50	84.50	2.00	1.70	0.003	0.70	0.02	1	45	215
18164	335065	8079512	2360	CH1		84.50	86.50	2.00	1.70	0.003	0.25	0.01	1	31	197
18165	335064	8079514	2360	CH1		86.50	88.50	2.00	1.70	0.003	0.25	0.01	1	64	171
18166	335063	8079515	2360	CH1	End Channel Sample	88.50	90.50	2.00	1.70	0.003	0.25	0.03	1	163	250
18173	335154	8079540	2350	CH2	Start Channel Sample	0.00	2.00	2.00	1.73	0.003	0.70	0.01	1	62	106
18174	335153	8079542	2350	CH2		2.00	4.00	2.00	1.73	0.003	0.50	0.02	1	134	195
18175	335152	8079544	2350	CH2		4.00	6.00	2.00	1.73	0.003	0.25	0.01	1	41	137
18176	335151	8079545	2350	CH2		6.00	8.00	2.00	1.73	0.003	0.70	0.03	1	47	178
18177	335150	8079547	2350	CH2		8.00	10.00	2.00	1.73	0.005	2.60	0.05	1	47	97
18178	335149	8079549	2350	CH2		10.00	12.00	2.00	1.73	0.005	3.20	0.27	1	93	141
18179	335147	8079550	2350	CH2		12.00	14.00	2.00	1.73	0.003	0.60	0.01	1	107	174
18181	335146	8079551	2350	CH2		14.00	16.00	2.00	1.73	0.003	1.20	0.03	1	89	176
18182	335144	8079553	2350	CH2		16.00	18.00	2.00	1.73	0.003	0.25	0.01	1	36	170
18183	335144	8079555	2350	CH2		18.00	20.00	2.00	1.73	0.003	0.70	0.01	1	40	138
18184	335142	8079556	2350	CH2		20.00	22.00	2.00	1.73	0.003	2.10	0.03	1	13	148
18185	335142	8079557	2350	CH2		22.00	22.40	0.40	0.35	0.005	10.60	0.72	1	31	698
18186	335141	8079558	2350	CH2		22.40	24.40	2.00	1.73	0.003	3.70	0.38	1	129	409
18187	335140	8079560	2350	CH2		24.40	26.40	2.00	1.73	0.003	0.25	0.01	1	42	175
18188	335139	8079561	2350	CH2		26.40	28.40	2.00	1.73	0.003	0.25	0.01	1	34	98
18189	335138	8079563	2350	CH2		28.40	30.40	2.00	1.73	0.005	0.25	0.01	1	20	90
18190	335137	8079565	2350	CH2		30.40	32.40	2.00	1.73	0.003	0.60	0.02	1	14	45
18191	335135	8079565	2350	CH2		32.40	34.40	2.00	1.73	0.003	0.25	0.00	1	5	31
18192	335133	8079565	2350	CH2		34.40	36.40	2.00	1.73	0.003	0.25	0.00	1	1	28
18193	335131	8079564	2350	CH2	End Channel Sample	36.40	38.40	2.00	1.73	0.003	0.70	0.01	1	3	27
18194	335118	8079562	2350	CH2A	Start Channel Sample	0.00	2.00	2.00	1.70	0.003	0.25	0.02	1	35	166
18195	335116	8079563	2350	CH2A		2.00	4.00	2.00	1.70	0.003	0.50	0.01	1	88	171
18196	335115	8079565	2350	CH2A		4.00	6.00	2.00	1.70	0.003	0.70	0.01	1	47	109
18197	335114	8079566	2350	CH2A		6.00	8.00	2.00	1.70	0.003	0.25	0.00	1	87	200
18198	335112	8079567	2350	CH2A		8.00	10.00	2.00	1.70	0.003	0.25	0.02	1	44	159
18199	335110	8079568	2350	CH2A	End Channel Sample	10.00	12.00	2.00	1.70	0.003	0.25	0.01	1	17	18
18200	335141	8079518	2355	CH3	Start Channel Sample	0.00	2.00	2.00	1.65	0.021	2.80	1.73	1	136	345
18202	335140	8079519	2355	CH3		2.00	4.00	2.00	1.65	0.003	2.80	0.02	1	45	134
18203	335139	8079520	2355	CH3		4.00	4.25	0.25	0.21	0.077	5.10	4.73	1	54	255
18204	335138	8079521	2355	CH3		4.25	6.25	2.00	1.65	0.005	3.40	0.43	1	46	206
18205	335138	8079522	2355	CH3		6.25	6.50	0.25	0.21	0.017	9.50	4.35	1	71	758
18206	335137	8079523	2355	CH3	End Channel Sample	6.50	8.50	2.00	1.65	0.005	3.10	0.17	1	16	273
18207	335122	8079512	2360	CH4	Start Channel Sample	0.00	1.50	1.50	1.23	0.003	0.90	0.02	1	96	186
18208	335122	8079513	2360	CH4		1.50	3.00	1.50	1.23	0.005	3.10	0.65	1	127	203
18209	335121	8079514	2360	CH4		3.00	4.00	1.00	0.82	0.013	4.70	1.41	1	94	185
18210	335120	8079515	2360	CH4	End Channel Sample	4.00	5.50	1.50	1.23	0.025	3.40	2.18	1	182	264
18240	337396	8079489	2277	CH5	Start Channel Sample	0.00	0.20	0.20	0.20	0.695	91.60	0.50	157	66700	15650
18242	337395	8079487	2276	CH5	End Channel Sample	0.00	1.00	1.00	1.00	0.663	294.00	1.35	83	110500	24600
18339	335634	8079449	2318	CH6	Start Channel Sample	0.00	2.00	2.00	1.77	0.005	1.00	0.15	1	104	245
18341	335636	8079448	2318	CH6		2.00	4.00	2.00	1.77	0.036	1.00	1.74	1	144	325
18342	335637	8079447	2318	CH6		4.00	6.00	2.00	1.77	0.003	0.80	0.01	1	67	238
18343	335639	8079446	2318	CH6		6.00	8.00	2.00	1.77	0.003	0.80	0.01	1	56	180
18344	335641	8079446	2318	CH6		8.00	10.00	2.00	1.77	0.005	2.00	0.32	2	2110	178
18345	335643	8079446	2318	CH6		10.00	11.00	1.00	0.89	0.092	4.50	2.23	4	2920	211
18346	335644	8079446	2318	CH6		11.00	12.00	1.00	0.89	0.035	1.40	0.78	1	1540	196
18347	335645	8079446	2318	CH6		12.00	13.00	1.00	0.89	0.026	2.30	0.31	1	547	289
18348	335646	8079446	2318	CH6		13.00	14.00	1.00	0.89	0.003	1.30	0.01	1	120	207
18349	335647	8079445	2318	CH6		14.00	15.00	1.00	0.89	0.009	6.10	0.28	1	236	209
18350	335648	8079445	2318	CH6		15.00	16.00	1.00	0.89	0.010	6.70	0.21	1	100	237
18351	335648	8079446	2318	CH6		16.00	17.00	1.00	0.89	0.029	4.40	0.96	1	157	200
18352	335649	8079446	2318	CH6		17.00	18.00	1.00	0.89	0.017	3.30	0.19	1	91	334
18353	335650	8079446	2318	CH6		18.00	19.00	1.00	0.89	0.025	4.30	0.45	1	97	335
18354	335651	8079446	2318	CH6		19.00	20.00	1.00	0.89	0.003	2.10	0.05	1	62	176
18355	335652	8079447	2318	CH6		20.00	21.00	1.00	0.89	0.003	1.60	0.02	1	94	182
18356	335653	8079447	2318	CH6		21.00	22.00	1.00	0.89	0.011	2.50	0.19	1	236	297
18357	335654	8079448	2318	CH6		22.00	23.00	1.00	0.89	0.119	3.10	1.48	1	530	433
18358	335654	8079449	2318	CH6		23.00	24.00	1.00	0.89	0.006	1.90	0.24	1	322	240
18359	335655	8079449	2318	CH6		24.00	25.00	1.00	0.89	0.007	2.80	0.44	1	470	296
18361	335656	8079450	2318	CH6		25.00	26.00	1.00	0.89	0.013	3.10	0.97	1	478	318
18362	335656	8079451	2318	CH6		26.00	27.00	1.00	0.89	0.012	2.00	0.49	1	148	296
18363	335658	8079452	2318	CH6		27.00	29.00	2.00	1.77	0.003	0.50	0.01	1	69	295
18364	335659	8079453	2318	CH6		29.00	31.00	2.00	1.77	0.003	0.25	0.01	1	42	243
18365	335661	8079454	2318	CH6		31.00	33.00	2.00	1.77	0.003	0.25	0.01	1	23	231
18366	335663	8079455	2318	CH6	End Channel Sample	33.00	35.00	2.00	1.77	0.003	0.25	0.00	1	55	296
18367	335699	8079710	2260	CH7	Start Channel Sample	0.00	0.70	0.70	0.70	0.003	0.25	0.01	1	46	208
18368	335699	8079711	2260	CH7		0.70	1.80	1.10	1.10	0.141	8.20	2.89	1	823	847
18369	335698	8079712	2260	CH7		1.80	2.90	1.10	1.10	0.535	25.20	8.70	1	283	873
18370	335698	8079713	2260	CH7	End Channel Sample	2.90	3.50	0.60	0.60	0.003	5.90	0.03	1	103	238
18371	335727	8079710	2279	CH8	Start Channel Sample	0.00	2.00	2.00	2.00	0.003	0.25	0.02	1	144	356
18372	335727	8079705	2279	CH8		2.00	4.00	2.00	2.00	0.003	0.25	0.03	1	44	152
18373	335727	8079709	2279	CH8		4.00	5.50	1.50	1.50	0.008	0.80	0.12	1	61	237
18374	335727	8079711	2279	CH8		5.50	6.50	1.00	1.00	0.027	4.90	0.80	1	246	611
18375	335727	8079707	2279	CH8	End Channel Sample	6.50	8.00	1.50	1.50	0.003	0.25	0.02	1	35	140
18376	335750	8079686	2267	CH9	Start Channel Sample	0.00	2.00	2.00	2.00	0.003	1.50	0.01	1	47	209
18377	335749	8079687	2267	CH9		2.00	3.50	1.50	1.50	0.342	8.40	0.65	1	121	407
18378	335748	8079688	2267	CH9		3.50	4.50	1.00	1.00	0.124	14.20	1.12	1	160	512
18379	335747	8079689	2267	CH9		4.50	5.50	1.00	1.00	0.021	7.80	0.31	1	99	230
18381	335746	8079690	2267	CH9		5.50	6.50	1.00	1.00	0.039	8.10	0.32	1	354	323
18382	335746	8079690	2267	CH9		6.50	7.50	1.00	1.00	0.048	6.20	0.25	1	216	230
18383	335745	8079691	2267	CH9	End Channel Sample	7.50	8.50	1.00	1.00	0.046	5.20	0.45	1	122	447
18384	335754	8079657	2270	CH10	Start Channel Sample	0.00	2.00	2.00	2.00	0.010	3.10	0.13	1	438	219
18385	335753	8079658	2270	CH10		2.00	4.00	2.00	2.00	0.003	7.20	0.02	1	808	147
18386	335751	8079659	2270	CH10		4.00	6.00	2.00	2.00	0.031	3.50	0.10	1	615	184
18387	335749	8079660	2270	CH10	End Channel Sample	6.00	8.00	2.00	2.00	0.003	2.00	0.01	1	68	120

 

APPENDIX 1

Table 4 Cinto Rock Sample Geochemical Assay Results

Sample Number	East Coord	North Coord	Elevation	Au ppm	Ag ppm	Cu %	Mo ppm	Pb ppm	Zn ppm
18001	335743	8081059	2323	0.003	0.25	0.001	0.5	15	81
18002	335693	8080995	2296	0.003	0.25	0.001	0.5	8	9
18003	335416	8080766	2466	0.003	0.25	0.001	2	4	12
18004	335522	8080930	2512	0.015	0.5	0.002	146	210	20
18005	335393	8080772	2561	0.003	0.25	0.002	1	14	117
18006	335272	8080633	2399	0.003	0.25	0.002	2	11	27
18007	335138	8080492	2521	0.003	0.25	0.002	0.5	18	64
18008	335010	8080349	2494	0.003	0.25	0.002	1	16	35
18009	334880	8080184	2492	0.003	0.25	0.002	3	9	42
18010	334732	8080008	2439	0.003	0.25	0.002	2	20	28
18011	334632	8079876	2431	0.003	0.25	0.002	1	19	102
18012	334627	8079817	2450	0.003	0.25	0.003	3	3	13
18013	334481	8079741	2320	0.003	0.25	0.003	1	18	65
18014	334364	8079568	2288	0.003	0.25	0.003	1	16	65
18015	334271	8079436	2473	0.003	0.25	0.003	0.5	11	66
18016	334114	8079254	2456	0.003	0.25	0.003	1	27	87
18017	334007	8079144	2476	0.003	0.25	0.003	1	22	101
18018	334113	8079047	2457	0.003	0.25	0.003	0.5	14	112
18019	334252	8079170	2377	0.003	0.25	0.003	0.5	10	121
18020	334391	8079288	2518	0.003	0.25	0.003	1	16	79
18022	334525	8079415	2443	0.003	0.25	0.003	1	15	65
18023	334517	8079445	2382	0.003	0.25	0.003	1	24	82
18024	334628	8079602	2437	0.003	0.25	0.004	1	38	100
18025	334731	8079754	2483	0.003	0.25	0.004	0.5	6	41
18026	334889	8079906	2360	0.003	0.25	0.004	0.5	38	154
18027	334797	8080021	2460	0.003	0.25	0.004	27	14	22
18028	335048	8080077	2487	0.003	0.25	0.004	0.5	18	87
18029	335191	8080217	2476	0.003	0.25	0.004	0.5	10	96
18030	335342	8080361	2459	0.003	0.25	0.004	3	18	26
18031	335360	8080396	2295	0.003	0.25	0.005	0.5	11	82
18032	335429	8080556	2567	0.003	0.25	0.005	3	40	82
18033	335540	8080661	2430	0.003	0.25	0.005	0.5	15	99
18034	335683	8080796	2472	0.003	0.25	0.005	1	19	62
18035	335816	8080939	2498	0.003	0.25	0.005	0.5	11	71
18036	335618	8080633	2614	0.003	0.25	0.005	1	11	85
18037	335955	8080852	2349	0.003	0.25	0.005	1	203	133
18038	335851	8080686	2435	0.003	0.25	0.005	2	15	61
18039	335695	8080562	2510	0.003	0.25	0.005	3	7	64
18041	335590	8080386	2373	0.003	0.25	0.006	0.5	24	73
18042	335439	8080217	2410	0.003	0.25	0.006	1	17	92
18043	335306	8080084	2427	0.003	0.25	0.006	1	41	172
18044	335165	8079900	2510	0.003	0.25	0.006	0.5	21	158
18045	335035	8079778	2670	0.503	0.25	0.007	2	19	115
18046	334945	8079631	2496	0.003	0.25	0.007	1	26	54
18047	334774	8079462	2429	0.494	0.25	0.007	3	5	118
18048	334648	8079339	2429	0.003	0.25	0.007	3	11	11
18049	334524	8079162	2608	0.003	0.25	0.007	4	6	25
18050	334406	8079013	2446	0.003	0.25	0.008	0.5	15	109
18051	334306	8078810	2513	0.003	0.25	0.008	0.5	31	110
18052	334407	8078773	2375	0.003	0.25	0.008	1	21	111
18053	334559	8078877	2453	0.003	0.25	0.009	0.5	118	176
18054	334690	8078981	2476	0.003	0.25	0.009	1	14	81
18055	334814	8079180	2567	0.003	0.25	0.009	8	6	30
18056	334931	8079344	2475	0.003	0.25	0.009	1	10	80
18057	335922	8080561	2445	0.003	0.25	0.01	2	12	69
18058	335839	8080423	2554	0.003	0.25	0.01	2	13	112
18059	335724	8080241	2400	0.003	0.25	0.01	1	11	58
18060	335552	8080088	2403	0.003	0.25	0.01	0.5	17	169
18061	335552	8080088	2466	0.003	0.25	0.011	0.5	11	57
18062	335476	8079939	2399	0.003	0.25	0.011	1	9	86
18063	335335	8079753	2487	0.003	0.25	0.011	1	28	110
18064	334580	8078593	2477	0.005	0.25	0.011	1	16	96
18065	334716	8078747	2487	0.003	0.25	0.012	1	25	98
18066	334832	8079910	2511	0.003	0.25	0.012	1	8	87
18067	334994	8079050	2738	0.003	0.25	0.013	1	24	72
18068	334287	8079489	2653	0.003	0.25	0.016	3	18	98
18069	335203	8079640	2680	0.003	0.25	0.016	3	13	70
18070	334674	8079308	2610	0.005	0.25	0.016	9	107	147
18071	335072	8079182	2390	0.003	0.25	0.018	1	14	101
18072	335226	8079357	2418	0.003	0.25	0.018	2	13	96
18073	335357	8079505	2390	0.003	0.25	0.019	1	14	113
18074	335475	8079654	2545	0.003	0.25	0.019	0.5	12	107
18075	335631	8079800	2726	0.003	0.25	0.019	2	18	98
18076	335745	8079964	2507	0.003	0.25	0.02	1	14	91
18077	335871	8080110	2738	0.003	0.25	0.02	1	12	83
18078	335421	8080898	2541	0.003	0.25	0.021	2	20	98
18079	335323	8080910	2507	0.003	0.25	0.021	2	10	91
18081	335222	8079648	2458	0.003	0.25	0.043	2	11	100
18082	332909	8077932	2345	0.003	0.25	0.001	0.5	11	19
18083	332914	8077833	2330	0.003	0.25	0.001	0.5	12	21
18084	333000	8077617	2250	0.008	0.25	0.002	1	5	27
18085	335781	8079778	2259	0.01	1.1	0.131	0.5	67	247
18086	335312	8080109	2378	0.017	2.4	0.519	2	25	108
18087	335370	8080093	2379	0.003	0.25	0.003	0.5	31	84
18088	335378	8080079	2400	0.003	0.25	0.015	1	17	70
18089	335464	8080000	2365	0.003	0.25	0.007	0.5	19	73
18090	335092	8079956	2419	0.003	0.25	0.181	1	110	456
18091	335069	8079973	2469	0.003	0.25	0.003	0.5	24	86
18092	335641	8079888	2398	0.022	2	0.742	1	26	73
18093	335688	8079782	2351	0.003	0.25	0.001	1	16	49
18094	335533	8079702	2402	0.003	0.25	0.001	1	28	57
18167	335058	8079520	2360	0.003	0.25	0.005	0.5	51	101
18168	335058	8079520	2360	0.003	0.25	0.004	0.5	47	175
18169	335054	8079521	2360	0.003	0.25	0.014	0.5	81	309
18170	335053	8079521	2360	0.003	0.25	0.007	0.5	62	256
18171	335049	8079520	2360	0.003	0.25	0	1	44	250
18172	335048	8079520	2360	0.003	0.25	0	0.5	39	243
18211	336036	8079982	2302	0.005	0.25	0.019	0.5	13	122
18212	336679	8079999	2414	0.005	0.25	0.013	1	12	46
18213	336818	8079994	2460	0.003	0.25	0.011	1	15	41
18214	337082	8079908	2490	0.005	0.25	0.013	1	17	68
18215	337086	8079996	2500	0.003	0.25	0.019	2	17	103
18216	337342	8079997	2380	0.003	0.25	0.017	1	17	87
18217	337614	8080020	2370	0.009	3.3	0.102	1	1910	7770
18218	337706	8079708	2330	0.006	3.3	0.636	4	18	127
18219	335015	8079447	2428	0.003	0.7	0.015	1	462	255
18221	337218	8079841	2460	0.145	17.1	0.03	1	1580	671
18222	337257	8079883	2410	0.003	0.25	0.016	3	21	53
18223	337837	8079403	2071	0.006	0.25	0.014	5	97	91
18224	336389	8079870	2379	0.023	0.25	0.035	0.5	78	273
18225	336664	8079841	2393	0.003	0.25	0.018	1	11	86
18226	336425	8079534	2269	0.003	0.25	0.018	0.5	17	104
18227	336405	8079481	2254	0.003	0.25	0.005	1	6	33
18228	337198	8079725	2402	0.003	13.4	0.018	1	11	80
18229	337501	8079797	2277	0.009	0.25	0.014	2	9	61
18230	337317	8079686	2337	0.005	2.8	0.038	1	4620	2330
18231	337479	8079845	2310	0.003	0.25	0.03	2	25	72
18232	337615	8079691	2246	0.003	0.25	0.017	2	26	88
18233	337724	8079531	2181	0.003	0.25	0.014	1	14	88
18234	336165	8079238	2206	0.003	0.25	0.013	1	24	52
18235	336237	8079206	2151	0.007	0.25	0.024	0.5	8	88
18236	336307	8079117	2157	0.005	0.25	0.024	0.5	7	99
18237	336085	8079392	2211	0.012	1	0.188	2	260	262
18238	337432	8079262	2263	0.003	0.25	0.013	1	16	87
18239	337479	8079231	2253	0.003	0.5	0.01	1	18	86
18244	337399	8079369	2267	0.003	16.4	0.034	21	2130	300
18245	336960	8079540	2331	0.003	0.25	0.017	1	66	96
18246	336938	8079542	2329	0.003	0.25	0.016	1	42	90
18247	336823	8079383	2244	0.003	0.25	0.015	1	32	87
18248	336735	8079410	2241	0.003	0.25	0.015	1	20	83
18249	336694	8079224	2137	0.003	0.25	0.016	1	27	95
18250	337227	8079544	2387	0.003	0.25	0.018	2	22	89
18251	337399	8079377	2263	0.024	17.8	0.307	1	955	5380
18252	336465	8079471	2230	0.003	0.25	0.002	0.5	57	87
18253	337399	8079404	2255	0.173	303	0.364	9	29500	2570
18254	337401	8079403	2254	0.023	11.4	0.056	11	4100	2610
18255	337399	8079377	2263	0.308	201	0.588	216	42800	23900
18256	337404	8079375	2262	0.215	34.3	0.06	23	5400	7120
18257	337406	8079375	2260	0.009	13.1	0.048	2	1380	2530
18258	337409	8079375	2259	0.003	1.4	0.489	3	41	102
18259	337837	8079403	2086	0.007	0.25	0.014	6	139	117
18261	337282	8079596	2369	0.003	0.25	0.068	6	312	418
18262	337381	8079605	2322	0.093	90.8	0.212	8	16350	5860
18263	337481	8079545	2280	0.003	0.25	0.019	1	40	101
18264	337460	8079502	2262	0.008	1.2	0.027	1	268	459
18265	337407	8079496	2277	0.119	136	0.389	9	87200	1140
18266	337397	8079446	2257	1.985	232	1.06	83	100500	26100
18267	337413	8079337	2267	0.203	168	1.22	7	43500	8800
18268	335901	8079535	2200	0.003	0.7	0.036	0.5	135	416
18269	335778	8079692	2245	0.003	0.25	0.026	1	49	119
18270	336959	8079836	2419	0.003	0.25	0.016	2	23	110
18271	336835	8079674	2317	0.003	0.25	0.014	2	42	96
18272	336542	8079704	2248	0.003	0.25	0.012	1	23	91
18273	336090	8079544	2251	0.003	0.25	0.017	1	16	98
18274	337750	8079607	2193	0.003	0.25	0.016	1	19	78
18275	336558	8079086	2124	0.005	0.25	0.02	1	25	103
18276	336441	8079224	2129	0.003	0.25	0.028	1	24	99
18277	336567	8079369	2176	0.003	0.25	0.016	1	27	135
18278	336305	8079402	2189	0.003	0.25	0.032	1	16	109
18279	336055	8079434	2170	0.006	0.6	0.03	3	29	138
18280	336086	8079279	2136	0.003	0.25	0.022	1	17	120
18282	335913	8079208	2161	0.003	0.7	0.019	1	198	523
18283	336020	8079064	2175	0.003	0.25	0.026	1	14	114
18284	336839	8079090	2077	0.003	0.25	0.009	1	14	97
18285	335601	8079645	2330	0.003	0.25	0.003	0.5	39	101
18286	335634	8079541	2316	0.003	0.25	0.002	1	90	173
18287	335473	8079534	2307	0.003	0.25	0.003	0.5	15	140
18288	335516	8079392	2259	0.003	0.25	0.019	1	21	172
18289	335796	8079103	2203	0.003	0.25	0.008	2	18	78
18290	335751	8079404	2283	0.003	0.25	0.009	3	33	128
18291	335646	8079234	2232	0.003	0.25	0.021	1	14	106
18292	335781	8079223	2195	0.007	0.25	0.226	1	8	73
18293	335981	8079461	2167	1.175	1.4	1.115	13	16	328
18294	335567	8079481	2283	0.017	2.2	0.886	2	22	79
18295	335573	8079381	2248	0.012	0.25	0.689	1	22	95
18296	334669	8079194	2491	0.003	0.25	0.006	6	19	45
18297	334697	8079165	2494	0.003	0.25	0.005	1	6	40
18298	335095	8079112	2435	0.005	0.25	0.003	2	122	37
18299	334810	8079337	2478	0.003	0.25	0.004	0.5	10	51
18301	335177	8080251	2437	0.003	0.25	0.009	0.5	9	83
18302	335213	8079191	2385	0.003	0.25	0.004	4	8	75
18303	335245	8079077	2389	0.003	0.25	0.01	1	23	88
18304	335518	8079062	2335	0.003	0.25	0.004	0.5	8	25
18305	335372	8079222	2326	0.003	0.25	0.004	0.5	16	64
18306	335623	8080275	2382	0.003	0.25	0.006	1	9	69
18307	335987	8080548	2546	0.003	0.25	0.022	2	11	96
18308	335978	8080757	2594	0.003	0.25	0.021	1	9	92
18309	335731	8080423	2390	0.003	0.25	0.007	1	13	97
18310	335069	8079068	2432	0.003	0.25	0.001	0.5	1	29
18311	335453	8080121	2364	0.003	0.9	0.012	3	1160	168
18312	335315	8079985	2364	0.003	0.25	0.002	0.5	56	157
18313	335243	8079922	2383	0.003	0.25	0.006	0.5	29	105
18314	335082	8079806	2430	0.003	0.25	0.008	0.5	16	113
18315	335208	8079780	2411	0.003	0.25	0.009	0.5	18	174
18316	335344	8079872	2400	0.003	0.25	0.007	0.5	11	98
18317	335593	8079963	2307	0.003	0.25	0.018	1	13	101
18318	335726	8080099	2354	0.003	0.25	0.007	1	28	149
18319	335344	8080262	2406	0.005	0.25	0.005	8	6	27
18320	334539	8079819	2510	0.003	0.25	0.002	0.5	16	82
18322	334404	8079645	2471	0.003	0.25	0.003	0.5	39	110
18323	334160	8079364	2510	0.003	0.25	0.009	1	43	97
18324	333762	8079044	2587	0.026	0.25	0.001	1	28	66
18325	334031	8079354	2515	0.003	0.25	0.011	1	30	119
18326	334180	8079493	2463	0.003	0.25	0.002	1	11	93
18327	334274	8079654	2475	0.003	0.25	0.003	1	33	130
18328	333730	8079340	2505	0.003	0.25	0.013	1	15	81
18329	333649	8079186	2521	0.003	0.25	0.007	1	79	338
18330	333519	8079027	2547	0.003	0.25	0.002	1	8	117
18331	333372	8078879	2525	0.005	0.25	0.002	1	45	30
18332	333380	8078751	2484	0.003	0.25	0.001	1	14	73
18333	333491	8078910	2533	0.003	0.25	0.003	1	15	84
18334	333624	8079041	2580	0.003	0.25	0.001	1	5	65
18335	333896	8079479	2496	0.003	0.25	0.011	1	12	103
18336	335796	8079654	2280	0.065	0.5	1.135	6	31	109
18337	335704	8079550	2323	0.883	2.1	8.31	9	51	194
18338	335781	8079579	2272	0.005	0.5	0.139	1	21	137
18388	336964	8079231	2192	0.003	0.25	0.015	1	13	73
18389	337103	8079401	2314	0.003	0.25	0.016	1	14	80
18390	337193	8079390	2315	0.003	0.5	0.775	2	21	75
18391	337241	8079256	2258	0.003	0.25	0.015	2	14	91
18392	337079	8079103	2153	0.005	0.25	0.017	1	18	89
18393	337419	8079439	2245	0.003	0.7	0.018	1	136	439
18394	337439	8079423	2242	0.017	1.8	0.019	1	852	1420
18395	337471	8079399	2231	0.108	54.3	0.325	3	2860	7000
18396	337506	8079385	2221	0.003	0.25	0.021	1	130	283
18397	337597	8079381	2181	0.003	0.25	0.016	1	99	608
18398	337770	8079378	2090	0.007	0.8	0.047	3	516	1730
18399	337817	8079393	2073	0.005	1	0.435	3	28	93
18400	337859	8079391	2063	0.003	0.25	0.017	1	10	84
18402	336255	8079239	2122	0.005	0.25	0.107	1	8	70
18403	336150	8079357	2174	0.003	0.25	1.135	2	102	382
18404	336132	8079288	2140	0.094	11.3	0.476	1	343	209
18405	335914	8079534	2117	0.04	0.7	0.312	4	16	88
18406	335698	8079405	2315	0.005	0.25	0.544	3	16	121
18407	337710	8079833	2287	0.007	0.25	0.014	1	67	220
18408	337726	8079686	2219	0.003	0.25	0.022	1	42	170
18409	337887	8079556	2131	0.003	0.7	0.235	3	15	110
18410	337964	8079453	2112	0.012	0.5	0.222	3	19	71
18411	337948	8079619	2099	0.003	0.25	0.01	2	62	126
18412	335658	8079880	2286	0.009	2.9	0.562	2	31	76
18413	336190	8079299	2146	0.017	0.5	0.761	7	16	157
18414	334522	8078985	2416	0.015	13.1	2.08	1	30	95
18415	336251	8079227	2160	0.003	0.25	0.022	1	10	86
18416	334825	8080399	2422	0.003	0.25	0.021	2	26	106
18417	334564	8080057	2494	0.003	0.25	0.007	1	26	125
18418	334423	8079973	2468	0.003	0.25	0.004	1	15	65
18419	334291	8079797	2468	0.003	0.25	0.004	1	17	83
18421	334146	8079642	2456	0.003	0.25	0.006	2	13	80
18422	334027	8079498	2456	0.003	0.25	0.005	1	10	74
18423	334425	8079799	2476	0.003	0.25	0.002	1	15	81
18424	334150	8079954	2412	0.003	0.25	0.006	2	28	125
18425	334010	8079819	2392	0.003	0.25	0.004	1	8	71
18426	333901	8079648	2408	0.003	0.25	0.007	3	4	53
18427	333765	8079482	2494	0.003	0.25	0.011	1	12	83
18428	333659	8079304	2486	0.003	0.25	0.006	2	14	58
18429	333489	8079148	2525	0.003	0.25	0.001	2	33	79
18430	333387	8079007	2532	0.003	0.25	0.003	1	19	57
18431	334739	8078883	2420	0.003	0.25	0.002	1	3	21
18432	333124	8078754	2491	0.003	0.25	0	1	13	20
18433	332967	8078624	2480	0.003	0.25	0	1	12	20
18434	332919	8078421	2458	0.003	0.25	0.002	1	18	36
18435	334100	8080189	2369	0.003	0.25	0.003	1	27	128
18436	333900	8079965	2355	0.003	0.25	0.001	5	9	15
18437	333377	8079368	2416	0.003	0.25	0.012	3	54	166
18438	333224	8079173	2380	0.003	0.25	0.003	1	13	63
18439	333108	8079026	2418	0.003	0.25	0.001	1	8	71
18440	332976	8078863	2415	0.003	0.25	0.001	1	64	132
18442	334802	8078656	2395	0.005	0.5	0.01	4	45	81
18443	334819	8078625	2395	0.009	0.25	0.011	4	21	41
18444	334784	8078614	2383	0.003	0.25	0.011	17	19	26
18445	332964	8079246	2322	0.006	0.25	0.002	1	11	45
18446	333277	8079516	2322	0.003	0.25	0.014	1	16	90
18447	333277	8079516	2322	0.005	0.25	0.011	1	17	98
18448	333536	8079832	2324	0.003	0.25	0.004	1	13	93
18449	332706	8078888	2363	0.003	0.25	0.001	1	46	89
18450	332598	8078713	2341	0.003	0.25	0	1	35	69
18451	332481	8078562	2359	0.003	0.25	0	1	30	44
18452	333628	8079146	2529	0.006	0.25	0.188	2	33	87
18453	332343	8078421	2321	0.005	0.25	0.001	1	18	17
18454	332227	8078285	2777	0.005	0.25	0.001	1	13	50
18455	332446	8078259	2361	0.003	0.25	0.001	1	11	32
18456	332603	8078420	2382	0.003	0.25	0	1	17	70
18457	332717	8078570	2421	0.005	0.25	0.001	1	21	37
18458	332842	8078765	2439	0.003	0.25	0.001	2	22	46
18459	333631	8078710	2439	0.003	0.25	0.001	1	21	45
18461	333514	8078571	2392	0.003	0.25	0.005	1	10	70
18462	333341	8078447	2370	0.003	0.8	0.002	5	12	13
18463	333232	8078273	2388	0.003	0.25	0.004	2	11	67
18464	332984	8078290	2409	0.003	0.25	0	8	7	15
18465	333130	8078446	2421	0.003	0.25	0.004	1	13	76
18466	333247	8078590	2414	0.003	0.25	0.006	2	16	62
18467	333442	8078676	2444	0.003	0.25	0	1	20	59
18468	333500	8078239	2313	0.003	0.25	0.001	2	7	15
18469	333625	8078468	2364	0.003	0.25	0.003	1	13	39
18470	333772	8078579	2388	0.003	0.25	0.001	1	13	46
18471	333896	8078720	2452	0.003	0.25	0.001	1	21	154
18472	333284	8078489	2374	0.005	0.25	0.005	8	12	43
18473	333036	8078497	2438	0.003	0.25	0	1	9	11
18474	333223	8077937	2381	0.003	0.25	0	1	14	23
18475	333368	8077812	2379	0.003	0.25	0.001	1	14	20
18476	333509	8077972	2339	0.003	0.25	0.001	1	9	30
18477	333647	8078115	2286	0.003	0.25	0.001	4	19	64
18478	333789	8078279	2356	0.003	0.25	0.002	1	20	96
18479	333933	8078432	2373	0.003	0.25	0.001	1	18	91
18480	334041	8078610	2419	0.003	0.25	0.002	1	97	120
18482	334150	8078697	2484	0.003	0.25	0.001	1	22	58
18483	334290	8078934	2438	0.005	0.25	0.001	1	3	42
18484	334279	8078581	2478	0.003	0.25	0.006	1	5	62
18485	334161	8078440	2407	0.003	0.25	0	1	104	115
18486	334028	8078302	2321	0.003	0.25	0.001	1	12	27
18487	333932	8078129	2299	0.003	0.25	0.001	1	13	74
18488	333783	8077959	2290	0.003	0.25	0	1	8	34
18489	333654	8077826	2272	0.003	0.25	0.001	1	11	52
18490	333526	8077655	2288	0.003	0.25	0	1	15	42
18491	333396	8077491	2249	0.003	0.25	0.001	1	6	10
18492	333588	8077699	2303	0.003	0.25	0	1	7	14
18493	333515	8077421	2220	0.003	0.25	0.001	2	8	14
18494	333664	8077535	2259	0.003	0.25	0.001	3	17	9
18495	333774	8077675	2224	0.003	0.25	0	2	9	41
18496	333931	8077812	2254	0.003	0.25	0.001	1	12	12
18497	334018	8077981	2268	0.003	0.25	0.001	1	19	50
18498	334152	8078128	2311	0.003	0.25	0	1	28	123
18499	334273	8078291	2354	0.003	0.25	0.002	1	11	33
18501	334405	8078423	2430	0.003	0.25	0.003	1	6	36
18502	334924	8078718	2407	0.005	0.25	0.007	1	18	66
18503	334835	8078579	2391	0.005	0.25	0.008	1	15	65
18504	334678	8078430	2337	0.003	0.25	0.005	1	14	103
18505	334588	8078301	2358	0.003	0.25	0.004	1	10	94
18506	334419	8078133	2369	0.007	0.25	0.007	6	16	78
18507	334295	8077956	2345	0.003	0.25	0.004	1	16	87
18508	333972	8077797	2237	0.003	0.25	0.001	1	6	25
18509	334039	8077365	2197	0.003	0.25	0.001	1	12	28
18510	334178	8077504	2203	0.003	0.25	0	1	16	40

 

APPENDIX 2

JORC Code, 2012 Edition – Table 1

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 representativity 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 a30 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.	333 rock chip and grab samples were collected in 2H 2024 from outcrops on an approximate 200 x 200m grid over an area of 9km2 in the northeast of the Cinto tenements. Within this area, where visible copper oxide mineralisation was observed, further samples were taken off- grid to outline zones of interest. Coordinate position and assay results of each sample are shown in Table 4, Appendix 1 of this ASX release. The samples are considered to be as representative as possible of the exposure albeit that, by their nature, chip and grab samples do not reflect the overall grade of mineralisation encountered. Samples were representatively hand-cobbed to approximately 2.5kg mass for lab submission. These samples complement 45 samples taken previously (see ASX Release dated 9 July 2024 ). Within the rock sampling grid, 152 channel samples were taken from 10 separate channels of maximum and minimum field length 90.5m and 1.20m respectively. A total of 219.10m of channels were sampled (field length – see below for true length). Channel samples were taken on visible mineralisation exposures that were created by old (>50 years) small-scale workings or gully erosion. Channels 1-4, 6, and 9-10 exhibited old workings that were channelled. Within constraints of practicality, channels were sampled to cross mineralisation strike at a high angle and were designed to represent true widths. The channel samples were adjusted from sampled length to true length where exposure configuration caused curvature of the channel. Channels 1-4 and 6 were adjusted in this manner from GIS plans. Channels 5 and 7-10 are considered linear in the field and were not adjusted. Channel samples were taken in consistent fashion to maintain representative samples. In areas with old workings, usually more friable, the channels were dug approximately 10-20 cm wide by 10-20cm deep. In areas of natural exposure, the channels were chipped to 20-30cm wide by 5-10cm deep. Bulk samples were collected on a tarp. Sample lengths were usually 1.0m or 2.0m, or as short as 0.20m in a vein. Coordinate position and assay results of each channel sample are shown in Table 3, Appendix 1 of this ASX release. The coordinates are considered the centrepoint of the channel sample.
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 historical or new drilling has been reported in this announcement.
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.	No drilling reported herein.
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 in this announcement. Rock chip and grab samples were logged and rock type lithologies, oxidation and quantities of, and types of, mineralisation noted. Channel samples are logged in a similar but continuous fashion to construct a strip log of the channel. All channels were logged, 10 in total, for a total of 219.10m of logging (field length) (100% logged).
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 representativity 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.	Systematic rock channel sampling was taken and separated on a tarp – usually up to 30-50kgs per linear metre. Samples were usually friable rock or chips of <3cm and were coned and quartered to produce samples of 3kgs for lab submission. Tarps and shovels/picks were cleaned after each sampling. Field duplicates were taken across a range of channel sample mineralisation and reported excellent correlation. The sample procedure and preparation is considered appropriate for the nature of the base metal mineralisation tested and its distribution throughout the sample. Rock chip and grab samples taken were considered to be of appropriate size and representativity to ascertain if copper and or precious metal mineralisation is present at the outcrops.
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 (e.g. standards, blanks, duplicates, external laboratory checks) and whether acceptable levels of accuracy (i.e. lack of bias) and precision have been established.	All rock chips were assayed by ALS in Lima. Methods used were total assay of sample: Preparation PREP31 Analysis Au-AA23 and ME-ICP61 Cu OG-62 for overlimit Cu >1% Pb OG-62 for overlimit Pb >1% Zn OG-62 for overlimit Zn >1% Ag OG-62 for overlimit Ag >100ppm OREAS standards, blanks, and field duplicates were inserted at appropriate intervals and reported within required ranges.
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.	All Solis data is verified by the Competent Person. Channel sample intersections have been checked by alternative company director with prerequisite experience. All data is stored in an electronic database and sample rejects are stored in company warehouses. Competent Person and alternative company director have visited the site during channel sampling and observed sampling techniques and quality control. Channel sample intersections and widths were established.
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.	All sample locations were captured using a handheld GPS in WGS84 19S. Rock and chip samples are points. Channel sample intervals have their centrepoint as their GPS location.
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.	No set sample spacing or pattern has been applied due to the preliminary nature of the sampling programme. Exposures of mineralisation were tested where found and not on a regular pattern. The distribution of the mineralisation allows commentary on potential scope of mineralisation but does not imply continuity.
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.	Channel sample orientation was designed to cross mineralisation at a high angle where possible and appropriate in the exposures. No bias has been introduced in current drilling and sampling.
Sample security	The measures taken to ensure sample security.	All samples are bagged onsite under supervision of Solis staff, all bags are then sealed and couriered to the relevant laboratories with all relevant submission documentation. All samples once received are logged into the lab and notice of each sample received is sent and cross checked with sample dispatch.
Audits or reviews	The results of any audits or reviews of sampling techniques and data.	There have been no detailed external audits or reviews undertaken. Solis has conducted an internal technical review and site visit by the Competent Person and the alternative company director.

 

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