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- W2386520009 abstract "Cretaceous marine red beds are widely developed in the Gyangze area,southern Tibet.The Chuangde Formation is one of the most typical formations in this area.In this paper,based on electron microprobe backscattered electron image and quantitative analysis,major elements and X-ray diffraction analysis,in combination with diffuse reflectance spectroscopy data before and after treated by CBD(Citrate Bicarbonate Dithionite),it was suggested that hematite was the only ferruginous oxide in red shales of the Chuangde Formation and the unique ferruginous oxide of red color,no other ferruginous oxides were found.Electron microprobe backscattered electron images showed that hematite occurs in two forms: poor-crystallinity and good-crystallinity.The redness variation of diffuse reflectance spectra before and after CBD treatment indicated that hematite of poor-crystallinity was much richer than that of good-crystallinity.The red color of red shales in the Chuangde Formation was mainly caused by finely dispersed poor-crystallinity hematite.Hematite was the product of co-deposition-early diagenesis,and ferric iron from which hematite was formed came from terrestrial input." @default.
- W2386520009 created "2016-06-24" @default.
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- W2386520009 date "2009-01-01" @default.
- W2386520009 modified "2023-09-23" @default.
- W2386520009 title "Color Genesis of Red Shales in Cretaceous Marine Red Beds from Gyangze,Southern Tibet" @default.
- W2386520009 hasPublicationYear "2009" @default.
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