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- W2393055545 abstract "The Mamaoke gold ore deposit is located in the Jiuzhaigou County, northwestern Sichuan Province. It is one of the important ore deposits in the triangle area of Shanxi Gansu Sichuan Provinces. The main gold bearing minerals include pyrite, arsenopyrite, stibnite, realgar, and limonite. There are two types of pyrite, which formed in the sedimentary diagenetic period and hydrothermal period. The former typically has framboidal texture, while the latter shows zoned texture . The gold content of pyrite with smaller grain size and anhedral shape is higher than that of those with larger grain size and euhedral shape. Stibnite and realgar occurring as micro disseminates normally have higher content of gold than those of massive ores. Limonite, formed in the supergenetic oxidation period, contains micro to super micro native gold. Studies of the gold bearing minerals in the Manaoke gold deposit show that the deposit formed in three different periods: sedimentary diagenetic period, hydrothermal period, and supergenetic oxidation period. The evolution of ore bearing hydrothermal fluids is characterized by stages. Sharp changes in physical chemical conditions of the ore bearing fluids are favorable for the gold precipitation." @default.
- W2393055545 created "2016-06-24" @default.
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- W2393055545 date "2002-01-01" @default.
- W2393055545 modified "2023-09-25" @default.
- W2393055545 title "CHARACTERISTICS OF THE GOLD-BEARING MINERALS AND THEIR SIGNIFICANCE TO THE ORE GENESIS OF THE MANAOKE GOLD DEPOSIT, NORTHWESTERN SICHUAN" @default.
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