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- W350126114 abstract "Baekun gold-silver deposit is an epithermal quartz vein that is filling the fault zone within Triassic or Jurassic foliated granodiorite. Mineralization is associated with fault-breccia zones and can be divided into two stages. Stage I which can be subdivided early and late depositional stages is main ore mineralization and stage II is barren. Early stage I is associated with wallrock alteration and the formation of sulfides such as arsenopyrite, pyrite, pyrrhotite, sphalerite, marcasite, chalcopyrite, stannite, galena. Late stage I is characterized by Au-Ag mineralization such as electrum, Ag-bearing tetrahedrite, stephanite, boulangerite, pyrargrite, argentite, schirmerite, native silver, Ag-Te-Sn-S system, Ag-Cu-S system, pyrite, chalcopyrite and galena. Fluid inclusion data indicate that homogenization temperatures and salinity of stage I range from NaCl, respectively. It suggest that ore forming fluids were cooled and diluted with the mixing of meteoric water. Also, Temperature (early stage I: $236~>380^{circ}C,;$ late stage $I: a atm., late stage I: .) deduced mineral assemblages from stage 1 decrease with paragenetic sequence. Sulfur ((early stage )), oxygen ((quartz: early stage , late stage )), hydrogen ( (quartz: early stage )) and carbon ( (calcite: late stage I)) isotope compositions indicated that hydrothermal fluids may be magmaticorigin with some degree of mixing of another meteoric water for paragenetic time." @default.
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- W350126114 date "2006-01-01" @default.
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- W350126114 title "Ore minerals and Genetic Environments from the Baekun Gold-silver Deposit, Republic of Korea" @default.
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