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- W2366195328 abstract "The Xuqiao silver ore deposit is situated in the southeastern part of the Anqing- Guichi mining camp in the mid-lower Yangtze River reaches metallogenetic belt,with silver reserve up to a medium size,mineralization being hosted in watershed quartz diorite,mainly stratoid ore body occurring in the interlayer fractures of the Ordovician Lunshan Formation and Tangshan Formation.Ore minerals include pyrite,sphalerite,galena,tetrahedrite,chalcopyrite,argentite,natural silver;gangue minerals are quartz and carbonate minerals;ore fabrics are substantially euhedral-anhedral,metasomatic,sparsely disseminated and stockworked;wall rock alteration is dominated by silication,carbonatation,skarnization and chloritization.The deposit has two mineralization epochs: hydrothermal epoch and supergene epoch,and the former is further divided into three stages,i.e.,skarn stage,quartz-sulfide stage and carbonate-sulfide stage;ore-forming fluid is predominantly magmatic hydrothermal fluid in the early period,and joined by precipitation later.Ore-forming material is mainly derived from magmatic hydrothermal fluid,with some contribution from strata.Ore formed at midlow temperature(208～259℃)leading to a mid-low hydrothermal silver polymetallic deposit and giving clues for deepseated ore prospecting in the ore district." @default.
- W2366195328 created "2016-06-24" @default.
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- W2366195328 date "2013-01-01" @default.
- W2366195328 modified "2023-09-23" @default.
- W2366195328 title "Geological features of the Xuqiao silver ore deposit and downward ore-prospecting direction in the ore district,Chizhou,Anhui" @default.
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