Abstract
Mesothermal gold mineralization at the Samdong mine (5.5–13.5 g/ton Au), Youngdong mining district, is situated in massive quartz veins up to 1.2 m wide which fill fault fractures within upper amphibolite to epidote-amphibolite facies, Precambrian-banded biotite gneiss. The veins are mineralogically simple, consisting of iron- and base-metal sulfides and electrum, and are associated with weak hydrothermal alteration zones (<0.5 m wide) characterized by silicification and sericitization. Fluid inclusion data and equilibrium thermodynamic interpretation of mineral assemblages indicate that the quartz veins were formed at temperatures between 425 and 190°C from relatively dilute aqueous fluids (4.5–13.8 wt. % equiv NaCl) containing variable amounts of CO2 and CH4. Evidence of fluid unmixing (CO2 effervescence) during the early vein formation indicates approximate pressures of 1.3–1.9 kbars, corresponding to minimum depths of ≈ 5–7 km under a purely lithostatic pressure regime. Gold deposition occurred mainly at temperatures between 345 and 240 °C, likely due to decreases in sulfur activity accompanying fluid unmixing. The δ34S values of sulfide minerals (-3.0 to 5.3 ‰), and the measured and calculated O-H isotope compositions of ore fluids (δ18O = 5.7 to 7.6‰; δ = −74 to −80‰) indicate that mesothermal gold mineralization at the Samdong mine may have formed from dominantly magmatic hydrothermal fluids, possibly related to intrusion of the nearby ilmenite-series, ‘Kimcheon Granite’ of Late Jurassic age.
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So, CS., Yun, ST. & Shelton, K.L. Mesothermal gold vein mineralization of the Samdong mine, Youngdong mining district, Republic of Korea. Mineral. Deposita 30, 384–396 (1995). https://doi.org/10.1007/BF00202281
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DOI: https://doi.org/10.1007/BF00202281