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- W2377689890 abstract "The formation of skarn-type ore deposits is closely related with geological structures.In this paper,the Tongshan Cu deposit in Anhui province is systematically studied,involving the geological structures that influence skarn deposit formation,such as faults,folds,unconformities and contact zones in the study area.The results show that structural activities run through the whole process involving magma intrusive emplacement,magmatic hydrothermal fluid activity,contact replacement and mineralization.The magmatic emplacement and the presence of ore bodies are mainly controlled by unconformities.Skarn mineralization zoning is different in vertical direction.In the shallow subsurface,the ore body primarily occurred in skarn within the contact zone between C-P limestone and Yanshanian dioritic complex.While at depth,the ore body is associated with intrusive emplacement in the form of hydrothermal fluid,followed by contact replacement and skarnization that caused mineralization.The joint ore-controlling of fault-contact zones resulted in reverse skarn mineralization zoning." @default.
- W2377689890 created "2016-06-24" @default.
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- W2377689890 date "2010-01-01" @default.
- W2377689890 modified "2023-09-26" @default.
- W2377689890 title "Ore-Controlling Structures and Their Influence on Mineralization of the Skarn Copper Deposit in Tongshan,Anhui Province" @default.
- W2377689890 hasPublicationYear "2010" @default.
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