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- W2362801008 abstract "Taking the Browns Cu-polymetallic deposit as an example,the authors study its geological and geochemical characteristics.It is believed that the Cu,Pb and Zn were enriched during hungery deposition stage, and formed a sedimentary-reformed deposit mineralized by brine effect of later basins.On the basis,the authors conclude the metallogenic regularity of this kind of Cu deposit by constrasting with the Zanbian copper belt(ZCB), Kupferschiefer copper belt in Poland,and Dongchuan copper belt in Yunnan of China.It is considered that the metallic minerals are commonly sourced from the underlying red-bed and weathered basement;the sulfur is from the evaporite and black shale/mudstone,and rarely from the ancient hydrocarbon reservoirs.The metallogenic fluid are mid-high salinity and intermediate temperate oxidized basin brine.The metallogenic minerals transport mainly as Cl-complex(CuCl_3~- ),and the driver force of fluid flow are tectonic activity,radiation heat and salt diapir can also lead to fluid transportation.Reduction is the main mechanism of metallic minerals precipitation,and in-situ organic matter is the main reducing agent.The metallic minerals combined with S and precipitated on oxidation-reduction interface,and mineralized during the basin evolution." @default.
- W2362801008 created "2016-06-24" @default.
- W2362801008 creator A5091280805 @default.
- W2362801008 date "2011-01-01" @default.
- W2362801008 modified "2023-09-26" @default.
- W2362801008 title "Genesis of sedimentary rock-hosted stratiform copper deposit——a case study on Browns Cu-polymetallic deposit,Australia" @default.
- W2362801008 hasPublicationYear "2011" @default.
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