Minsud encounters 555m at 0.43% Cu, 0.19 g/t Au, 4.80 g/t Ag including 44m at 1.12% Cu, 0.29 g/t Au and 9.52 g/t Ag at Chinchillones

In This Article:

TSXV: MSR

TORONTO, Feb. 14, 2024 /CNW/ - Minsud Resources Corp. (TSXV: MSR) ("Minsud" or the "Company"), is pleased to announce the receipt of assay results from eight (8) additional drillholes, which were completed as part of the ongoing Phase IV infill and scout drilling program at the Chita Valley Project, San Juan Province, Argentina.

Since the commencement of the Earn-in agreement with South32 Aluminium (Holdings) Pty Ltd ("South32") a wholly owned subsidiary of South32 Limited, a total of ninety-eight (98) drillholes have been completed to date, encompassing 63,168 metres. Assay results have been received from drillholes CHDH23-91 through CHDH23-98, which total 5,883 metres.

In 2023, Minsud completed 25,986.4 metres of diamond drilling. Of this, 16,148.4 metres were from scout drilling and 9,838.0 metres were from the infill drilling program.

Key highlights and associated figures are provided below. Summary of drilling results is shown in Table 1. Drillhole locations are shown in Map 1. Documented alteration and mineralization are shown in Map 2.

CHDH23-96 was drilled with an orientation of 315°/-65° to a depth of 801 metres:

  • Significant Drill Intercepts:

    • 555.0m @ 0.43% Cu, 0.19 g/t Au and 4.80 g/t Ag, from 246m depth.

      • including 44.0m @ 1.12% Cu, 0.29 g/t Au, 9.52 g/t Ag, from 462.0m depth.

  • Geology:

    • The drillhole was comprised of intercalated phreatomagmatic breccias and fine to medium grained porphyritic dacite. Dominantly matrix-supported, polymictic, advanced argillic-altered dacitic breccias with prominent porphyritic dacite and quartzite clasts. Significant mineralization occurs as minute, frequent sulphide disseminations and in high sulphidation veins hosting up to 5% pyrite-bornite-sphalerite-tennantite. Narrow intervals of high sulphidation veins with more than 50% sulphides (pyrite-chalcopyrite-sphalerite-galena; e.g., 456-457m).

    • This higher-grade intercept shows potential continuity with the high-grade intercepts from CHDH23-73, CHDH22-62, CHDH23-69, CHDH23-77, CHDH22-57 and CHDH23-81, all of which exhibit similar Cu-Au geochemistry.

    • This important Cu-Au body is apparently aligned WNW and coincident with the eastern edge of a late dome-diatreme complex.

    • This higher-grade Cu-Au zone is surrounded by Cu-Au-As high sulphidation mineralization implying this Cu-Au porphyry mineralization is linked to the Cu-Au-As high sulphidation (HS) mineralization.

CHDH23-91 was drilled with an orientation of 315°/-75° to a depth of 850 metres:

  • Significant Drill Intercepts:

    • 386.0m @ 0.27% Cu, 0.07 g/t Au and 3.19 g/t Ag, 200 ppm Mo, from 458.0m depth.

  • Geology:

    • Up to 530.3m, dominantly intercalated, clast-supported, phreatomagmatic breccia. The breccia body hosts mineralized clasts of dacitic composition, quartzites and early dioritic porphyry. There are intervals with late silicification and high sulphidation veins. Strongly silicified zones host up to 5% sulphides (pyrite-tennantite-sphalerite-molybdenite-chalcopyrite). A medium grained tonalite porphyry was encountered from 530m hosting stockwork, B+A and Mo veins with up to 5-7% sulphides (pyrite-chalcopyrite-molybdenite-sphalerite).