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- W2375010358 abstract "The clay mineral in uranium-bearing target strata of Lower Cretaceous in Hongshan area of Jiudong basin have been studied by scanning electron microscopy(SEM),X-ray diffraction(XRD),X-ray spectroscopy(EDX)and etc.The clay mineral is found mainly kaolinite,followed by chlorite.The source rocks of clastic rocks in target layer are mostly acidic magmatic rocks with alkaline metasomatism.The sources of kaolinite include both land-based source and the authigenic(alteration);the alteration belt of kaolinization(light colour zone)can be used as mainly criterion layer for prospecting uranium deposits in Hongshan area,and its thickness and intensity can be used as one of the evidence to judge the extent of uranium enrichment.The chlorite is mostly self-chlorite which was formed at different times to that of kaolinite and might be turned from the kaolinite.The study of clay minerals show that the weather in this area has experienced a gradual change from warm and humid to dry environent since Lower Cretaceous." @default.
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- W2375010358 date "2010-01-01" @default.
- W2375010358 modified "2023-09-24" @default.
- W2375010358 title "Study on the clay mineral in uranium-bearing target strata of Lower Cretaceous in Hongshan area, Jiudong basin" @default.
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