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- W2365781422 abstract "The Ordos basin is greatest one of the oil,natural gas pool,coal minee and uranium deposit collection in the same basin.This basin is component part of Archeozoic—Proterozoic crystalline basement and marine and lake sedimentary cover of Paleozoic group unite into North China Plate.On the Ordos basin was divided into Mesozoic—Cenozoic piedmont depression basin from North China in Mesozoic era.The Ordos basin of Mesozoic—Cenozoic era is undergoing three develop evolution stage from tableland basin, fault block and after basin .This paper make a concrete analysis of favourable condition of uranicum metallogenetic geological-geochemistry in Mesozoic—Cenozoic era basin. Theuranicum abundance of the host sandstone (4.71×10 -6～34.3×10 -6) is a few multiple-outstrip one quantitative stage higher than mean value of upper earth crust abundance. This paper expounds characteristics of petrology of host layer in Dongsheng uranium ore deposit and features of diagenetic-epigenetic-lowtemperature hydrothermal mineralization.The paper specifically analyses close relationship between green-bleaching mineralized alteration and uranium mineralization.The green and bleaching alteration has feature of the planer type distributed.They are hosted in upper plate and lower wall of uranium orebody respectively and have close relation of genesis to deep-basin gas.This mineralized alteration has characteristics of mineralization multi-epoch and multi-stage,complex mineral association paragenesis,diversified mineralized shape and characteristics of low-temperature hydrothermal mineralization(70～120℃).The sandstone-type uranicum ore deposit is the genesis of early stage of sedimentary pre-enrichment,succeed stage of leach of paleointerlayer oxidized zone and epigenetic deoxidation and epigenetic metasomatism." @default.
- W2365781422 created "2016-06-24" @default.
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- W2365781422 date "2006-01-01" @default.
- W2365781422 modified "2023-09-26" @default.
- W2365781422 title "The Metallogenic Condition and Epigenetic Alteration Mineralization of Dongsheng Uranium Deposit in the Inner Mongolia" @default.
- W2365781422 hasPublicationYear "2006" @default.
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