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- W2363364657 abstract "The ore-forming depth was a highly concerned factor for the predication of potential ore reserves of skarn Fe-Cu deposits in the middle Nanjing-Zhenjiang granite province,and was only estimated qualitatively by geological methods before.Sphalerite was found in these deposits as minor components and the authors preliminarily studied the properties in occurrence,paragenesis,basic chemical compositions as well as crystal structure of the minerals from representative mines of Funiushan(Cu),Anjishan(Cu),Tuanshan(S),Panlonggang(Fe-Cu) and Zhouwangcun(polymetallic).According to the occurrence and paragnosis,sphalerite was precipitated during the medium to terminal hydrothermal sulfide stage and two generations were present at least in some of these mines.The apparent color,morphology,crystalline habit,basic chemical composition and crystal structure of sphalerite are all varied regularly with the occurrence and paragenesis.Only the first generation sphalerite with dark brown color at Tuanshan and Funiushan mine was in equilibrium with pyrite and hexagonal pyrrohotite and met the demand of geobarometer application.The pressure calculated from the revised equation of sphalerite barometer was between 0.9 kPa and 1.2 kPa,equivalently to be the depth between 2.42km and 3.63 km,in a good accordance with the estimation from geological method.In reference to the recent achievement in deep prospecting in Daye,Hubei and Tongling,Anhui that was in the same metallogenetic belt with the middle Nanjing-Zhenjiang granite province the deep prospecting potential should be positive in this region." @default.
- W2363364657 created "2016-06-24" @default.
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- W2363364657 date "2009-01-01" @default.
- W2363364657 modified "2023-09-23" @default.
- W2363364657 title "Genetic mineralogical properties of sphalerite and discussions on its geobarometer application in skarn ore deposits in middle Ningzhen region" @default.
- W2363364657 hasPublicationYear "2009" @default.
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