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- W2365436483 abstract "Available pyrite occurs in sedimentary formation in Chongqing City.The pyrite that lies on the bottom of Longtan Formation(P3l) and Wujiaping Formation(P3w) accounts for about 92% of total.The ore-bearing formation and pyrite-formated deposited environment are studied and analyzed.The rocks are mainly kaolinization basic tuff,kaolinite claystone and grapholith,as well as coal-bed.Four areas rich in pyrite in Chongqing are northeast countries,east district,Huayingshan area and south of Chongqing.The material sources and its mineralization mechanism are discussed.The ferrum comes from Emeishan basalt and the sulfur is carried by seawater from different direction(north,northeast,south and east and so on).In the reducing environment,the pyrite was formed via recrystallization at the stage of diagenesis-epigenesis.The distribution regularity on thickness and grade are partly revealed and a primary metallogenic model is proposed.The sedimentary facies are mainly eluvial plain,marsh,tidal flat,and gulf,and the pyrite are chiefly formed in the transgression system." @default.
- W2365436483 created "2016-06-24" @default.
- W2365436483 creator A5051788465 @default.
- W2365436483 date "2013-01-01" @default.
- W2365436483 modified "2023-09-23" @default.
- W2365436483 title "Upper Permian Sedimentary Environment and Metallogenic Model of Pyrite in Chongqing" @default.
- W2365436483 hasPublicationYear "2013" @default.
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