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- W2360383857 abstract "The Pb-Zn deposits of Jianshui county in Yunnan Province,located in the south margin of Kunming folded belt,east Yunnan folding zone in Yangtze Paraplatform.The regional structure mainly in NE and EW of fracture and folding,structural lines of ore district are nearly in EW or NEE direction likely the regional structure lines,which is a monoclinal structure,SSE dip.This deposits in fault rupture zone during construction in Zaijieshan Formation of Devonian System.the stratigraphic inclination trend SSE-S and dip angle is 20~30°,the ithology is single,it is mainly composed of low gray-and-white and the low layered structure of micro-crystal-aplite.Mainly by the light grey,with its thin layer of dirt is a fine powder,and the crystalline-thick and thin,white powdered bulk of crystalline rock.The trend of the veins ore body is east-west.The major ore minerals are sphalerite,and a little galenite,with no other minerals,the gangue minerals is calcite.The ore deposit are controlled by NEE rift tectonic and the Zaijieshan Formation Dolostone of the Lower Devonian System.The ore-forming hydrothermal fluid via the fractured zones,it react with the active wall carbonate rocks in fractured zones by replacement,alteration and packing action.The useful mineral enriched and precipitated in favorable structures place.It formed this Pb-Zn Polymetallic Ore Deposit.and the results indicate that it is a hydrothermal(medium to low temperature type)." @default.
- W2360383857 created "2016-06-24" @default.
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- W2360383857 date "2012-01-01" @default.
- W2360383857 modified "2023-09-24" @default.
- W2360383857 title "Analysis on Metallogenetic Conditions of Shitouzhai Pb-Zn Deposits in Jianshui County,Yunnan Province" @default.
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