The role of weathering and soil formation in the evolution of the chemical composition of the earth's continental crust

被引：0
|
作者：
Dobrovol'skii, VV [1 ]
机构：
[1] Moscow State Pedag Univ, Moscow 119882, Russia
来源：
EURASIAN SOIL SCIENCE | 2002年 / 35卷 / 12期
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D O I：
暂无
中图分类号：
S15 [土壤学];
学科分类号：
0903 ; 090301 ;
摘要：
The influence of hypergenic transformation of silicate material on the chemical composition of the "granite" layer in the continental crust is discussed on the basis of data on its composition and structure. A relationship is established between the spreading of the first phytocenoses along with the beginning of soil formation and the accumulation of huge masses of kaolinite minerals being final products of silicate hypergenesis. It is shown that the epochs of weathering and soil formation that last for millions of years are confined to certain stages in global geotectonic cycles.
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页码：1247 / 1253
页数：7
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