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- W2389598971 abstract "The Tuwaishan gold deposit is located in the North-East part of the Gezhen auriferous shear zone in western Hainan province.It belongs to fragmentary altered rock gold deposit.The ore bodies occur mainly in migmatite in the hanging wall of shear zone.The study of fluid inclusion shows that quartz contains a great deal of primary fluid inclusions,i.e.,pure aqueous phase inclusion(I),aqueous two-phase inclusion(II),CO2-bearing three phase inclusion(Ⅲ)and pure CO2 inclusion(Ⅳ),with more than 70% of the fluid inclusion belonging to type(II).The ore-forming fluid belongs to NaCl-H2O type charactered by low-moderate temperature,low salinity and low density.The homogenization temperature of the three mineralization stages are 240～320℃,210～260℃,180～240℃;the salinity are 8%～10%,4%～8%,3%～8%,respectively,suggesting characteristics of low-meso temperatures and low salinity.The study of hydrogen and oxygen isotopic shows that the ore-forming fluid of Tuwaishan gold deposit were mainly derived from magmatic water and mixed with meteoric water.The increasing involvement of meteoric water resulted in falling of ore-forming temperature and salinity gradually." @default.
- W2389598971 created "2016-06-24" @default.
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- W2389598971 date "2008-01-01" @default.
- W2389598971 modified "2023-09-23" @default.
- W2389598971 title "Characteristics of Fluid Inclusion in the Tuwaishan Gold Deposit,Hainan Province and Their Geological Significances" @default.
- W2389598971 hasPublicationYear "2008" @default.
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