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- W2347767616 abstract "The formation of Chengmenshan copper deposit is associated with Changshan-Chengmenhu Lake anticline and NEE,NW and NNE trending fractures.The ore deposits mainly occur on the contact of the Yanshanian granodiorite porphyry with the carbonate rocks of Carboniferous,Permian and Triassic period, a part of the ore bodies was produced in the granodiorite porphyry.The ore-forming matters are origin in various sources or deep part sources.The deposit occurs in layer-like shape,bean pod shape,lens shape,belt-shape and mat shape. The ore genesis was analyzed according to the research of the characteristics of the deposit such as orebody shape,ore component,structure and texture,country rock alteration etc.It is concluded that the Chengmenshan copper deposit is a postmagmatic meso-epithermal deposit which was formed by several times' intrusion of intermediate-acidic calcium-alkali series magma of the late stage of Early Yanshanian period and the early stage of Late Yanshanian period,giving rise to the formation of so called three in one copper deposit,namly Karst type,massive sulfide type and porphyry type deposit that occur together." @default.
- W2347767616 created "2016-06-24" @default.
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- W2347767616 date "2007-01-01" @default.
- W2347767616 modified "2023-09-23" @default.
- W2347767616 title "Geological characteristics of Chengmenshan copper deposit,Jiangxi and its ore genesis" @default.
- W2347767616 hasPublicationYear "2007" @default.
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