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Geochemical Characteristics of the Fluid Inclusions Trapped in Primary Gypsum of the Lop Nor Basin
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作者 MA Lichun TANG Qingfeng +1 位作者 WANG Xin SUN Xiaohong 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2016年第1期382-383,共2页
Objective The Lop Nor Basin is a very important Quaternary potash-formation basin in China. It is a typical sulphate- potash brine mine with an average grade of 1.4% (KC1) in underground concentrated brines. It is e... Objective The Lop Nor Basin is a very important Quaternary potash-formation basin in China. It is a typical sulphate- potash brine mine with an average grade of 1.4% (KC1) in underground concentrated brines. It is extraordinary that the reservoir of potassium-rich brines is glauberite stratum rather than halite rock. The anomalous potassium enrichment, advanced in relative early stage of lake evolution (sulphate stage), has attracted much attention in the recent twenty years. Many researchers consider that there may be other source supply besides the Tarim River. 展开更多
关键词 Geochemical characteristics of the Fluid inclusions Trapped in Primary Gypsum of the Lop Nor Basin EVP
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Geochemical Characteristics of the Ore-forming Fluids of the Haigou Gold Deposit, Jilin
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作者 Li Yinqing Institute of Mineral Deposits, C AGS, Beijing 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 1994年第3期283-297,共15页
The quartz in the Haigou gold deposit contains a great abundance of three-phase CO2-NaCl-H2O and two-phase CO2-rich inclusions, which are associated with two-phase NaCl-H2O ones. The ore-forming fluids, which were ric... The quartz in the Haigou gold deposit contains a great abundance of three-phase CO2-NaCl-H2O and two-phase CO2-rich inclusions, which are associated with two-phase NaCl-H2O ones. The ore-forming fluids, which were rich in CO2, are classified into two types with two different sources: the high-salinity CO2-rich NaCl-H2O fluid derived from magmatic hydrothermal solution, and the low-salinity NaCl-H2O fluid from ancient meteoric water. The optimum conditions for gold mineralization are 220-300℃ for the temperature, 4-20 MPa for the fluid static pressure, 1-3 km for the mineralization depth, 2-7 w (NaCl)/10-2 for the fluid salinity, and 0.644 g/cm3 for the total density. The fluid was in a critical or supercritical state at the initial stage of mineralization, and it boiled and was unmixed with CO2 and NaCl-H2O in the climax of mineralization, leading to the decomposition of Au-chlorine complexes and the bulk precipitation of Au.The type, association, homogenization temperature and composition (CO2/H2O value etc.) are the microscopic criteria for distinguishing the auriferous quartz vein from the barren quartz 展开更多
关键词 monzonitic granite characteristics of fluid inclusion BOILING UNMIXING
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