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- W2363453492 abstract "SWIR 49.6°E hydrothermal field is the first discovered active field on the Southwest Indian ridge(SWIR) by the Chinese R/V Da Yang Yi Hao in 2007,which followed the earlier discovery of strong hydrothermal plume anomalies along this section of the SWIR in 2005.In this study,the mineralogy and mineral chemistry of the sulfide from this field were carried out.There are two distinct ore types,Zn-rich sulfide and Fe-rich sulfide.The dissertation porous structures,chalcopyrite diseasestructures,lamellae exsolution structures,and homologous overgrow structures are extensive in the sulfide ores.According to the mineral composition,the ore minerals can be classified into Fe-S series,Zn-S series,Cu-Fe-S series,Cu-S series and native metal series(Au,Cu,W).Based on the characteristics of mineral in the sulfide samples,two mineralization stages have been identified.Stage I,Zn-rich sulfide stage,the main mineral assemblages are sphalerite-pyrite-chalcopyrite and the temperature of ore-forming fluid is relatively low;Stage II,Fe-rich sulfide stage,the main mineral assemblages are pyrite-marcasite-sphalerite,and the ore-forming temperature is relatively high.The sulfides formed in early stage have been reworked by the late stage fluid." @default.
- W2363453492 created "2016-06-24" @default.
- W2363453492 creator A5090266163 @default.
- W2363453492 date "2011-01-01" @default.
- W2363453492 modified "2023-09-24" @default.
- W2363453492 title "Mineralogy of Sulfides from Ultraslow Spreading Southwest Indian Ridge 49.6°E Hydrothermal Field and Its Metallogenic Significance" @default.
- W2363453492 hasPublicationYear "2011" @default.
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