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也论成都粘土的成因
引用本文:汪波,聂前勇,王运生,张建永.也论成都粘土的成因[J].地质灾害与环境保护,2002,13(1):54-56,64.
作者姓名:汪波  聂前勇  王运生  张建永
作者单位:1. 成都理工大学环境与土木工程学院,成都,610059
2. 成都世纪电脑责任有限公司,成都,610000
3. 四川省交通厅公路勘察设计院,成都,610041
基金项目:地质灾害防治与地质环境保护国家专业实验室基金项目
摘    要:为了解成都粘土的成因机制,在总结前人资料的基础上,从分析成都粘土的分布、结构、矿物组成等特征入手,客观地展示了成都粘 本质,进而将其与我国北方的马兰黄土和长江中下游的下蜀粘土之间的特性进行比较以及对龙门山和成都平原第四纪晚更新世的古环境的分析,最终得出典型的成都粘土的成因是属于风成“黄土”的结论。

关 键 词:成因  风成黄土  成都粘土  古环境  结构  矿物组成
文章编号:1006-4362(2002)01-0054-03

DISCUSSION ON THE GENETIC MECHANISM OF CHENGDU CLAY
WANG Bo ,NIE Qian yong ,WANG Yun sheng ,ZHANG Jian yong.DISCUSSION ON THE GENETIC MECHANISM OF CHENGDU CLAY[J].Journal of Geological Hazards and Environment Preservation,2002,13(1):54-56,64.
Authors:WANG Bo  NIE Qian yong  WANG Yun sheng  ZHANG Jian yong
Institution:WANG Bo 1,NIE Qian yong 2,WANG Yun sheng 1,ZHANG Jian yong 3
Abstract:In order to study the genetic mechanism of Chengdu clay, the authors made analysis on the characteristics of Chengdu clay, such as distribution, structure, mineral constituent and so on, and objectively interpreted the essence of Chengdu clay in this paper on the basis of the studies on Chengdu clay in past decades. Then the paper compared Chengdu clay with Malan loess in North of China and Xiashu clay in middle-lower reaches of Changjiang (Yangtze) River and analyzed the paleo-environment in upper Pleistocene of Quaternary. The authors draw a conclusion that Chengdu clay is typically a kind of aeolian soil.
Keywords:Chengdu clay  genetic mechanism  aeolian loess
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