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- W2361584745 abstract "The Tianshengqiao Fe deposit is formed in Late Cambrian metamorphic rock series,which is in relation to the metasomasis of rising deep thermal fluid with carbonate rock and evidently controlled by the lithological character,horizon and structure.The genesis of this ore deposit is related with the metasomasis of rising thermal fluid of a blind acid rock body,which belongs to the Fe deposit of skarn type." @default.
- W2361584745 created "2016-06-24" @default.
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- W2361584745 date "2009-01-01" @default.
- W2361584745 modified "2023-09-23" @default.
- W2361584745 title "THE TIANSHENGQIAO SKARN FE DEPOSIT IN ZHENKANG" @default.
- W2361584745 hasPublicationYear "2009" @default.
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