
长江中游荆江流域环境演变及两湖平原盆地形成过程
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
Hu Dongsheng1,2,3、Zhang Huajing4、Xu Bing5、Gou Qingmei1、Yu Xuefeng2、Tian Xinhong3、Liu Weiguo2、An Zhisheng2、Zhang Guowei3
通过区域地质调查资料和地球卫星遥感解译技术对长江中游荆江流域及两湖平原盆地进行环境演 变及形成过程的综合研究,揭示了华中地块在全球新构造运动中发生的拉分运动对地表过程的影响,阐明了 流域水系和区域环境及平原盆地的同步演化关系,探讨了山-盆-原-江-湖-河耦合系统及环境演化的 地球动力学机制。
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.
长江中游荆江流域 / 两湖平原 / 环境演变过程 / 山-盆-原-江-湖-河耦合系统
Jingjiang River Valley of middle reaches of Yangtze River / Twain -Hu (Jianghan - Dongting) Plain / process of environment evolvement / mountain -basin -plain -river -lake -rivulet’s coupling system
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