| 庐山红色泥砾泥石流成因商榷 |
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| 引用本文： | 彭汉兴.庐山红色泥砾泥石流成因商榷[J].冰川冻土,1990,12(1):87-90. |
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| 作者姓名： | 彭汉兴 |
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| 作者单位： | 河海大学 南京 |
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| 摘 要： |
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| 关 键 词： | 泥石流 红色 泥砾 成因 |
Disecussion on the Formatation of the Debris Flow of the Red Bounder Clay in the Lushan |
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| Peng Hanxing.Disecussion on the Formatation of the Debris Flow of the Red Bounder Clay in the Lushan[J].Journal of Glaciology and Geocryology,1990,12(1):87-90. |
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| Authors: | Peng Hanxing |
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| Abstract: | The forming processes of the red bounder clay in the Lushan Mount include depos-itting and weathering after it. The properties of the bounder clay in this area, such as the chemical compasition, clay and gravel composition, were changed greatly because of weathering. The characteristics of the red bounder clay, that formed in the middle pleistocene can't be compared with those of the debris flow formed at present. Thus the usual argument is untenable on the formatation of the debris flow of the red bounder clay in the Lushan Mount. |
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| Keywords: | Lushan red bounder clay debris flow |
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