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- W2365613237 abstract "Garnet is a common mineral in most skarn deposits.The morphology,structure,composition,end-members and the mineralization of garnet in the central part of Ningzhen region are researched through the ways of situ observation,optical microscope,SEM,X-ray diffraction,EDX and the chemical analysis for ore-forming metallic elements.The result shows that the garnet belongs to grossular-andradite series.The garnet in Cu skarn deposits all belong andradite subspecies and it contains less Cu in Cu skarn deposits than the unmineralized zone.It is considered that the content of ore-forming metallic elements in garnet is due to the enrichment or decentralization of ore-forming metallic elements in skarn stage.Under the condition that the ore-forming metallic elements is same from magmatic differentiation,if the ore-forming metallic elements was enriched in garnet during skarn stage,it is not good for mineralization,whereas the garnet contains less ore-forming metallic elements but the ore-forming hydrothermal has more ore-forming metallic elements which are in favor of mineralization.It is concluded that the ore-forming metallic elements content of garnet can not be used as a guide in prospecting skarn deposits." @default.
- W2365613237 created "2016-06-24" @default.
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- W2365613237 date "2009-01-01" @default.
- W2365613237 modified "2023-09-23" @default.
- W2365613237 title "RESEARCH ON RELATIONSHIP BETWEEN MINERALIZATION AND GARNET IN SKARN IN CENTRAL PART OF NINGZHEN AREA" @default.
- W2365613237 hasPublicationYear "2009" @default.
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