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- W2374551385 abstract "The West Sichuan Plateau is located in the southeast margin of the Tibet Plateau,where the climate is mainly influenced by the Indian southwest summer monsoon and the Tibet Plateau monsoon.Major elements of loess-paleosol from the sequence of S0-S2 stratigraphy of the Garze A section are measured by X-Ray Fluorescence Spectrometry.The results show that the content of SiO2,Al2O3,Fe2O3,MgO,K2O,MnO and TiO2 vary from low to high values with significant change cycles,which varies with the alternately superimposition of loess layer and paleosol layers,however,the pattern of Ca is opposite.The chemical properties of Si,Al,Fe,Mg,K,Mn,Ti but Ca show a similarity during the process of chemical weathering.There are good correlations between elements of Fe,Mn,K,Al,Ti and the clay(2～8 μm) and the silt(30～64 μm) in loess,suggesting that the distribution of major elements is mainly controlled by the grain size of loess in the region." @default.
- W2374551385 created "2016-06-24" @default.
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- W2374551385 date "2010-01-01" @default.
- W2374551385 modified "2023-09-23" @default.
- W2374551385 title "Geochemical Characteristics of Major Elements of Ganzi loess in the Western Sichuan Province" @default.
- W2374551385 hasPublicationYear "2010" @default.
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