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- W2357551623 abstract "Sulfide multimetal deposit in Yindongzi is a sedimentary eruption ore deposit, since upper adding and alteration is very weak. It preserves hydrothermal synsedimentary feature perfectly and makes integral record of evolvement sequence of hydrothermal fluid activity, so it is an ideal inartificial laboratory to study basin ancient fluid.In longitudinal way, hot water sedimentary body in mine changes into a series of small rhythm laminea and constitutes an integral structural bed of cycling whose hot water sedimentary layer thickness is from small to large to small. This structural bed of cycling is composed of three parts, the bottom is carbonic phyllite in which bearing sphalerite, the middle is No13 main stripped rich orebody, and the top is Fedolomite phyllite in which bearing galenite, which reflects the evolvement sequence of hydrothermal fluid activity. Meanwhile, the content of Al2O3,MgO,Na2O and K2O and the ratios of Fe and Mn to Ti, SiO2 to Al2O3, SiO2 to MgO, SiO2 to K2O, the variety of scopolite's component and sulfur isotopic composition in pyrite and galenite change with similar cycling pattern in hydrothermal sedimentary cycling rock." @default.
- W2357551623 created "2016-06-24" @default.
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- W2357551623 date "2003-01-01" @default.
- W2357551623 modified "2023-09-28" @default.
- W2357551623 title "Geochemical characteristics and hydrothermal deposit cycling of sedimentary eruption ore deposit" @default.
- W2357551623 hasPublicationYear "2003" @default.
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