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- W2390942136 abstract "Chahantonggu sag which located above the Paleozoic granitoid basement is a inter-mountain small sag in the northwest of.The Xishanyao group in middle Jurassic forms large area of thickly sandstone type uranium mineralization of very low-grade ore.The paper discusses the uranium metallogenetic as follows:the uranium source,the producing formation,the tectonic evolution,the oxidized zone,the uranium mineralized characteristics and so on.The sag wasrich in uranium source,Xishanyao group is carbon-bearing elastic rock building,steady sand body has more carbon,the ore-bearing layer is the second,third and forth rock sections.They have two subesidences and accept sedimentations in J2 and E3,two uplifts and suffer corrode in J3-E2 and N1-Q in tectonic evolution course.the Xishanyao group had pianar dive oxidized with the first and fifth rock sections,partial oxidized zone with the second,third and forth rock sections.The uranium mineralization from the zone of oxidized-reduced transition,which major in sandstone type,a few mudstone type.Deficiency is the time of interstratified oxidized mineralization in the Chahantonggu sag may be very short,mineralization mater disperses in the huge sand bodies,Uranium mineralization reached grade are present thin layer only,and has considerable resources reserves of uranium.The compaction and tectonic extrusion after mineralization made the sand body cementation and further densification." @default.
- W2390942136 created "2016-06-24" @default.
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- W2390942136 date "2012-01-01" @default.
- W2390942136 modified "2023-09-25" @default.
- W2390942136 title "Analysis of uranium metallogenic characteristics of the Chahantonggu sag of Kumishi basin,Xinjiang" @default.
- W2390942136 hasPublicationYear "2012" @default.
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