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Strategic Study of CAE >> 2010, Volume 12, Issue 1

On the environment evolvement of Jingjiang River Valley and the forming processes of Twain-Hu Plain Basin in the middle reaches of the Yangtze River

1. College of Resources Environmental Science, Hunan Normal University, Changsha, 410081, China;

2. State Key Laboratories of Loess and Quatenary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710075, China;

3. State Key Laboratories of Continental Dynamics, Northwest University, Xi'an, 710069, China;

4. College of Chemistry and Chemical Engineering, Hunan Normal University, Changsha, 410081, China;

5. College of Ocean Geosciences, Chinese Ocean University, Qingdao, Shandong 226071, China

Funding project:中国科学院地球环境研究所黄土与第四纪地质国家重点实验室开放基金项目( SKLLQG0701);湖南省重点学科建设项目(ZRDL0701);西北大学大陆动力学国家重点实验室开放基金项目(DL2006001) Received: 2008-11-26

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Abstract

Based on the investigation data of region geology and the remote sensing interpretation technique of earth satellite, the environment evolrement and the forming process of Jingjiang River in the middle reaches of Yangtze River and the basin of Twain-Hu (Jianghan-Dongting) Plain Baisn were comprehensively researched, it revealed the influence of the pull -apart activity in Huazhong (Middle China) Craton in new global construct movement to surface processes, there are clarified the relation synchronously evolvement from with the valley water system ,to surface processes the region environment and the basin of Twain-Hu(Jianghan -Dongting) Plain, the discuss into the earth dynamic mechanism for the mountain -basin -plain -river -lake -rivulet's coupling system and the environment evolvement.

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