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- W2388503396 abstract "Compared with other MVT deposits,the lead-zinc sulfide deposits gathering in the north margin of Quren carbonate basin,Guangdong Province,China,have mineralization particularity. The deposit strata and fault structure geochemistry,rare earth elements(REE),sulphur isotope,lead isotope and fluid inclusion geochemistry were discussed for understanding the source of the ore-forming metal,fluids and the mineralization processes in Fankou-type lead-zinc deposit. The strata,fault structure and REE results show that this type deposit experiences pyrite and lead-zinc mineralization processes,the former gets closer provenance contact with limestone,while ore metal of the latter does not come directly from ore-hosting carbonate rocks,but gets from basin deep fluid transferred up by NE,NW faults,and is slightly modified by intermediate-basic magmatism. Lead and sulphur isotope geochemistry of ores and related geological samples shows that lead comes mainly from basement clastic formation,partly from crust remelting type granitic magma,little from carbonate rocks; sulphur is mainly from carbonate rocks,only a litter from crustal magma. Sphalerite fluid inclusions components,salinity and temperature results reveal that lead-zinc hydrothermal mineralization exists ancient geothermal anomaly,and basement clastic aquifer and Yanshanian granite are involved in lead-zinc mineralization. Fankou-type MVT lead-zinc deposit in this research area can be classified as two-hydrothermal superimposition-transformation lead-zinc deposit after geochemical characteristics of ore deposits being analyzed synthetically." @default.
- W2388503396 created "2016-06-24" @default.
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- W2388503396 date "2013-01-01" @default.
- W2388503396 modified "2023-09-26" @default.
- W2388503396 title "Geochemistry of Fankou-type MVT lead-zinc sulphide deposit in northern margin of Quren basin,Guangdong Province,China" @default.
- W2388503396 hasPublicationYear "2013" @default.
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