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- W2372060367 abstract "Yushiwa iron deposit is one of the medium-sized skarn-type deposits in Han-Xing area.Based on the studied on homogeneous temperature,salinity and gas-liquid ingredients of fluid inclusion,the results show that the ore fluids belong to mid-high temperature(210–450 ℃),mid-high salinity(18.0%–20.0%) and the K+-Na+-Ca2+-Mg2+-Cl--SO42--F-system.Gas composition of the fluid inclusion is dominant by H2O,and secondly by CO2,CH4 and H2.The mineralization fluids may originate primarily from magmatic hydrothermal fluid,and part of them from precipitation.Multi-emplacement activities of rock bodies provide heat source for ore-forming process in Yushiwa iron deposit,and with precipitation iron enrichment mineralization occurs." @default.
- W2372060367 created "2016-06-24" @default.
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- W2372060367 date "2013-01-01" @default.
- W2372060367 modified "2023-09-26" @default.
- W2372060367 title "Fluid Inclusions Characteristics of Yushiwa Iron Deposit,Wuan County,Hebei Province,China and Its Geological Significance" @default.
- W2372060367 hasPublicationYear "2013" @default.
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