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Chemical characteristics of clay minerals in the sediments from the Yellow River and the Changjiang River

机译:黄河,长江沉积物中粘土矿物的化学特征。

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摘要

THE characteristics of clay minerals are controlled by the characters of weathered mother rock and the weathering environments in source area. The characteristics of clay minerals of the Yellow River should be different from those of the Changjiang River because the characters of mother rock and the weathering environments in the drainage area of the Yellow River are quite different from those in the drainage area of the Changjiang River, so it is important to find a difference between the characteristics of clay minerals of the Yellow River and the Changjiang River for the study of sedimentology in the China Sea, specially for analysing the source of sediments in a given area and for plotting of provenances in the China Sea, In recent years, a relative study has been done by some writers. In this note, we analyze the chemical characteristics of clay minerals from the Yellow River and the Changjiang River in order to reveal the differences between the clay minerals of the Yellow River and those ofthe Changjiang River.
机译:粘土矿物的特性受风化母岩的特性和源区的风化环境的控制。黄河的黏土矿物的特性应该与长江的黏土的特性有所不同,因为黄河流域的母岩特征和风化环境与长江流域的差异很大,因此,找到黄河和长江黏土矿物的特征之间的差异对于研究中国海的沉积学,特别是分析给定区域的沉积物来源和绘制物源图很重要。中国海,近年来,一些作家进行了相关研究。在本文中,我们分析了黄河和长江黏土矿物的化学特征,以揭示黄河和长江黏土矿物之间的差异。

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