Contributors Corner Eps 12-Digging Deeper: Why the Big Players Are Betting on Junior Miners"
Big-cap mining companies are facing a major problem: dwindling reserves and a lack of new discoveries. Instead of taking on early-stage risk themselves, they're increasingly turning to junior explorers to do the heavy lifting—making small caps the new hunting ground for future supply.
In this episode of Contributors Corner, we unpack this shift with Paul Sun, CEO of Eminent Gold (TSXV: EMNT), a junior explorer operating in Nevada that's already caught market attention with its high-potential targets and technical team stacked with major mining pedigrees.
Paul shares how this surge in strategic interest is reshaping the junior space, what big players are really looking for, and how companies like Eminent are positioning themselves to benefit. With capital tighter than ever, majors are becoming more selective, and the juniors with real assets and seasoned leadership are standing out.
🎙️ Listen in as we explore how this top-down investment trend is creating new momentum for juniors and why it might just mark the start of a major shift in mining's capital landscape.
🌍 Learn more about Eminent Gold at eminentgoldcorp.com
Check out our past issues of Contributors Corner where Michael Succurro from Spark Financial and Lyndsay Malchuk break open the topics that matter most for your portfolio and Bundeep Singh from Fineqia gives us all the 4-1-1 on crypto and blockchain
DISCLAIMER: These conversations are packed full of useful knowledge for your portfolio decisions, and remember these are the opinions of our own, with vested interests in particular assets and companies. Always be sure you speak with your Financial Advisor and know your own risk tolerance. For full disclaimer information, please click here
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Thus, the 32m @ 0.34% Cu and 58 ppm Mo within a wider interval of 120m @ 0.21% Cu and 77 ppm Mo from 22m demonstrated that the resource base of the supergene-enriched, open-pittable PSU deposit has the potential to be substantially expanded and upgraded. Drillhole PSUDH25-156 (315°azimuth and 60°dip; total depth of 261m) intersected highly oxidised (jarosite-goethite) diorite porphyry to 53m and at depth, transitional to a sulfidic zone hosting porphyry-related veinlets (quartz-pyrite-chalcopyrite-molybdenite; B- and D-type veins) with the sulfides replaced by chalcocite and digenite. At 142m, the dioritic porphyry body is traversed by quartz stockworked zone of white mica-quartz-pyrite-chalcopyrite-molybdenite altered dacitic intrusion. Drillhole PSUDH-157 (315°azimuth and60°dip; total depth of 252m) intersected dioritic porphyry from 3m characterised by a mixed zone of iron oxides (jarosite-goethite-hematite) with preserved sulfidic veins hosting pyrite-chalcopyrite and molybdenite. From 45m, the chalcocite-digenite replacement of sulfides become apparent. At depth from 98m through to 252m (end of hole) the lithologies become multi-phased with dacitic, andesitic and dioritic intrusion phases hosting copper sulfides. Drillhole PSUDH-158 (135°azimuth and 60°dip; total depth of 314.2m) confirmed the extension of the higher-grade molybdenum zone (>200 ppm Mo) hosted in diorite porphyry and affected by supergene chalcocite-digenite in the mixed oxide-sulfide zone commencing from 25m through to 84m below surface. Thence through to the end of the drillhole, the dioritic host rocks exhibit phyllic (white mica-quartz-pyrite) overprint over potassic (secondary biotite-K-feldspar-magnetite) hosting quartz-molybdenite-chalcopyrite stockworked quartz veining (B-type porphyry-related veinlets). The total iron mapped from Landsat 8 imageries (see Map 2 below) demonstrates coherent available total iron over PSU and extends farther south for at least 1.7 kilometres along strike. This significant total iron footprint is also coincident with structurally perturbed area, along the hanging wall to the NS-trending thrust fault, providing ideal environment for the development and transport of acidic fluids required for the dissolution and enrichment (vertical or lateral transport) of copper-bearing sulfides in the weathered profile. Interestingly, the high total Fe also affected the older Permian granitoids immediately to the east. Table 1: Scout Diamond Drilling Program – Summary of Significant Results (1) The true thicknesses are unknown REGIONAL TARGETING HIGHLIGHTS Extensive geological, geophysical and geochemical synthesis confirms highly prospective >>6km-long, >2.0km-wide, ENE- to NE-trending polymetallic Miocene-aged corridor (Map 3) The detailed mapping at the Placetas area confirmed the presence of coeval dioritic and dacitic lithologies, similar to the host rocks hosting the Chinchillones polymetallic deposit. At Chinchillones, the high sulfidation mineralization, polymetallic intermediate sulfidation veins, linear breccias and porphyry-related B-, A-, C-type veins are apparently controlled by NE-, EW-trending faults occurring in a NE-trending, 2.0km-long and 0.9km-wide elongated polymetallic zone. These controlling structures, considered as potentially fluid and magma pathways, are also present at the Placetas area. At Placetas Central, compelling drill-ready targets (Map 4) The results from the grid soil survey (206 samples;100m interval grid) highlights coherent coincident, at least 1km-long, 0.5km-wide Cu-Mo-Au anomalies. Importantly these multi-element anomalies coincide with an ENE-trending faulted zone separating the dioritic rocks in the NW with the dacitic rocks in the SE. This setting is highly reminiscent to the controls at the Chinchillones polymetallic deposit There is a significant fault-controlled EW-trending magnetite-destructive elongated "doughnut" coincident with a mapped dioritic porphyry intrusion, emplaced amongst an older, bigger dioritic body. This mapped younger body is interpreted to represent a protruded dyke coming off a younger, productive intrusion at depth. At PSU Surrounds, valid targets to test continuity of Cu-Mo-Au mineralization and the presence of other intrusion centres (Maps 5 and 6) The compiled surface geochemistry, magnetic-depleted zones and mapping around the PSU area indicate the southern area to the PSU requires drill-testing. The under-tested southern continuation of the supergene-enriched PSU (Porphyry Chita Sur) Cu-Mo-Au deposit measures 1.7km x 1.4km which can host substantial deposit/s. The total iron mapped from Landsat 8 imageries demonstrates coherent available total iron over the PSU surrounds and extends farther south for more than one kilometre. NEXT STEPS: Completion of the planned 5400m PSU expansion drilling A planned US$7.3 million budget from July 2025-June 2026 will include these exploratory activities: an MT survey over 13,5kms x 8.0kms area encompassing all the principal target areas testing of the compelling drill-worthy targets at Placetas Central and PSU south prospect areas expanded soil and rock geochemical survey, in conjunction with detailed mapping of the Chinchillones-Placetas corridor Identification of targets based on the thorough integration of the results from geology-geochemical and geophysical surveys COMMENT Mr Ramiro Massa, Director at Minsud Resources, commented: "These latest exploration results further validate the scale and strategic significance of the Chinchillones–Placetas corridor. With multiple mineralized centres and substantial untested extensions, we believe this emerging district holds significant potential for the delineation of multiple mineralized systems. Together with South32, we remain fully committed to systematically advancing exploration and unlocking long-term value from this high-quality asset located in one of Argentina's most mining-friendly jurisdictions". Quality Assurance/Quality Control All core samples were cut and prepared on-site at the project area. The sample lengths were usually 2 m, except in areas with low recovery (loss areas, faults, etc.) and breaks from discrete principal geological features (e.g., vein, vein breccia). Drill core sizes of the drillholes included in this report: CHDH25-150 (HQ to 490.8m;NQ to 675m); CHDH25-151 (all HQ to 500m); CHDH25-152 (all HQ to 501m; NQ to 600m); CHDH25-153 (all HQ to 492.6m); CHDH25-154 (all HQ to 510m); PSUDH25-155 (all HQ to 321m); PSUDH25-156 (all HQ to 261m); PSUDH25-157 (all HQ to 252m); and PSUDH25-158 (all HQ to 314.2m). Cutting was carried out by trained MSA personnel. Cores were split using the industry-standard Corewise automatic circular diamond blade rotary saw in the middle of the core, around 1 cm away from the core orientation mark. Half-core and duplicate samples, including all fragments, were placed in labelled plastic bags. Each had the sample number and was sealed using plastic security straps. All core samples were submitted to the ALS Patagonia S.A. in Mendoza as the primary laboratory for sample preparation. This ISO 9001 accredited facility, with the prepared pulp samples sent to ALS Perú S.A. in Lima, Peru. The ALS Perú S.A. laboratory is accredited under ISO 9001:2008 and ISO 17025, ensuring compliance with international standards. The analytical protocols are outlined as follows: ME-MS61 and ME-MS61m: Multitrace analysis of 48 elements with a 4-acid digestion. A prepared sample (0.25 g) is digested with perchloric, nitric, and hydrofluoric acids to dryness. The residue is taken up in a volume of 12.5 mL of 10 % hydrochloric acid. The resulting solution is analyzed by ICP-AES. Results are corrected for spectral interelement interference. ME-OG62: For samples over-limit, analysis is with four acid digestion using conventional ICPAES analysis for Ag, As, Cu, Mo, S, Pb, and Zn. Fire Assay Procedure Au-AA24 (50g): Gold is analyzed using a conventional fire assay fusion method with Atomic Absorption Spectroscopy (AAS). Minsud followed industry standard procedures for the work with a quality assurance/quality control (QA/QC) program. Field duplicates, standards and blanks were included with all sample shipments to the principal laboratory. Minsud detected no significant QA/QC issues during review of the data. Qualified Person (QP) Statement The scientific and technical information in this press release has been compiled, reviewed and approved by Dr Renato Bobis, MAusIMM CP (Geo), part-time VP-Exploration of the Company, and is a qualified person as defined by Canadian National Instrument Bobis has sufficient experience relevant to the style of mineralisation and type of deposit under consideration and to the activity which he is undertaking to qualify as a Qualified Person. About the Chita Valley Project, San Juan Province The Chita Valley Project is a large exploration stage porphyry system with widespread porphyry style Cu-Mo-Au and polymetallic Ag-Pb-Zn mineralization hosted in multi-phased intrusions and country rocks with affiliated hydrothermal breccias. San Juan Province of Argentina has a robust mining sector and recognizes the important economic benefits of responsible development of its substantial mineral resource endowment. The Chita Valley Project is owned and managed by MSA, of which Minsud indirectly holds a 49.9% interest. The other 50.1% interest in MSA is owned by a wholly owned subsidiary of South32 Limited ("South32"). Minsud and South32 entered into a shareholders' agreement to govern the management and operation of MSA which will include further exploration. About Minsud Resources Corp. Minsud is a mineral exploration company focused on exploring its flagship Chita Valley Cu-Mo- Au-Ag-Pb-Zn Project, in the Province of San Juan, Argentina. The Company's shares are listed on the TSX-V under the trading symbol "MSR", and on the OTCQX under the symbol "MDSQF". About South32 Limited South32 Limited ("South32") is a globally diversified mining and metals company. The company's purpose is to make a difference by developing natural resources, improving people's lives now and for generations to come, and to be trusted by its owners and partners to realise the potential of their resources. South32 produces minerals and metals critical to the world's energy transition from operations across the Americas, Australia and Southern Africa and is discovering and responsibly developing its next generation of mines. South32 aspires to leave a positive legacy and build meaningful relationships with partners and communities to create brighter futures together. CAUTIONARY STATEMENT REGARDING FORWARD-LOOKING INFORMATION: This news release includes certain information that may constitute forward-looking information under applicable Canadian securities laws. Forward-looking information includes, but is not limited to, statements about strategic plans, spending commitments, future operations, results of exploration, anticipated financial results, future work programs, capital expenditures and objectives. Forward-looking information is necessarily based upon a number of estimates and assumptions that, while considered reasonable, are subject to known and unknown risks, uncertainties, and other factors which may cause the actual results and future events to differ materially from those expressed or implied by such forward-looking information including, but not limited to: fluctuations in the currency markets (such as the Canadian dollar, Argentina peso, and the U.S. dollar); changes in national and local government, legislation, taxation, controls, regulations and political or economic developments in Canada and Argentina or other countries in which the Corporation may carry on business in the future; operating or technical difficulties in connection with exploration and development activities; risks and hazards associated with the business of mineral exploration and development (including environmental hazards or industrial accidents); risks relating to the credit worthiness or financial condition of suppliers and other parties with whom the Company does business; presence of laws and regulations that may impose restrictions on mining, including those currently enacted in Argentina; employee relations; relationships with and claims by local communities; availability and increasing costs associated with operational inputs and labour; the speculative nature of mineral exploration and development, including the risks of obtaining necessary licenses, permits and approvals from government authorities; business opportunities that may be presented to, or pursued by, the Company; challenges to, or difficulty in maintaining, the Company's title to properties; risks relating to the Company's ability to raise funds; and the factors identified under "Risk Factors" in the Company's Filing Statement dated April 27, 2011. There can be no assurance that such information will prove to be accurate, as actual results and future events could differ materially from those anticipated in such information. Accordingly, readers should not place undue reliance on forward-looking information. All forward-looking information contained in this news release is given as of the date hereof and is based upon the opinions and estimates of management and information available to management as at the date hereof. The Company disclaims any intention or obligation to update or revise any forward-looking information, whether as a result of new information, future events or otherwise, except as required by law. Neither the TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release. SOURCE Minsud Resources Corp.
