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- W2380116404 abstract "There is a lot of geochemical research on red clay resulting from weathering in the Quaternary weathering crust of carbonate rocks in Guizhou Province. However,no research has been conducted on the Quaternary weathering crust geochemistry of expansive Neoproterozoic low-grade metamorphic regions in eastern Guizhou. In this paper the authors take the Neoproterozoic low-grade metamorphic weathering crust at Darong Brickyard of Congjiang as the subject of study to explore the distribution of trace elements in this system. Finally,it was discovered that this modern weathering crust profile and red clay resulting from weathering of carbonate stones show similar features that in the upper part of the weathering crust is developed limonite layers,and in the bottom Mn,Co,Mo,Cd,Cs,Ba,Tl,Pb,etc. are highly enriched,The increase of pH value plays a vital role in deposition and enrichment of various trace elements. The main cause that the study profile shows low trace element contents integrally might be that the parent rocks have a low background level of trace element contents and developed diaclases. On the basis of the magnitude of correlation,trace elements in the earth of Darong Brickyard weathering crust profile are cluster analyzed by SPSS software. There is,in cluster analysis p,an obvious principle that trace elements with the similar geochemical motility in the supergene-environment are classified as the same group." @default.
- W2380116404 created "2016-06-24" @default.
- W2380116404 creator A5011478376 @default.
- W2380116404 date "2010-01-01" @default.
- W2380116404 modified "2023-09-25" @default.
- W2380116404 title "Trace Element Distribution Characteristics and Correlation Analysis of Modern Weathering Crust Profile of Neoproterozoic Epimetamorphic Rocks in Darong,Congjiang County,Guizhou Province" @default.
- W2380116404 hasPublicationYear "2010" @default.
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