Formation and development of the structure of collapsing loess in China
Formation and development of the structure of collapsing loess in China
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DOI：
10.1016/0013-7952(88)90029-4
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发表时间：
1988-06
影响因子：
7.4
通讯作者：
G. Guorui
中科院分区：
文献类型：
--
作者：
G. Guorui
高光，1988。中国黄土崩塌构造的形成与发展。Eng。青烟。中文信息学报，25:235-245。众所周知，在中国，黄土微观结构的区域变化与湿陷性的总体趋势是相一致的，从西北到东南逐渐减少。这些差异与气候条件的变化是一致的。这表明黄土塌陷的构造与气候条件和地质环境密切相关。通过微观结构分析，可以认为中国崩塌黄土结构的形成和发展经历了黄土化阶段、形成阶段、发育阶段、退化阶段和粘土化阶段五个阶段。黄土的五个阶段在黄土高原不同地区有规律地存在。这也说明在现代气候条件下，中国黄土高原西北部塌陷性黄土仍在发育。而黄土高原东南部的黄土塌陷特征正在逐渐消失。
Gao, G., 1988. Formation and development of the structure of collapsing loess in China. Eng. Geol., 25: 235–245.It is well known that in China the regional variations in microstructure of loess are in phase with the overall tendency for collapsibility, gradually decreasing from the northwest to the southeast. These differences are consistent with variations in climatic conditions. This indicates that the structure of collapsing loess is closely related to the climatic condition and geological environment. Based on the microstructure analyses, it can be assumed that the formation and development of the structure of collapsing loess in China has undergone five stages: the loessization stage, the formation stage, the development stage, the degeneration stage and the clayization stage. The five stages of loess regularly exist in different regions of the Loess Plateau. This also shows that under the modern climatic condition the collapsing loess in the northwest of the Loess Plateau in China is still developing. However, the feature of collapsing loess is gradually disappearing in the southeast of the Loess Plateau.