| 青藏高原腹地第四纪地质环境演化的地球动力学机制 |
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| 引用本文： | 胡东生,张国伟. 青藏高原腹地第四纪地质环境演化的地球动力学机制[J]. 中国工程科学, 2011, 9(1): 81-88 |
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| 作者姓名： | 胡东生 张国伟 |
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| 作者单位： | 1. 湖南师范大学资源环境科学学院,长沙 410081; 2.西北大学大陆动力学国家重点实验室,西安 710056;西北大学大陆动力学国家重点实验室,西安 710056 |
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| 基金项目： | 中国可可西里地区国家重点科学考察项目（D2000204）;湖南省重点学科建设项目（D2007001）;西北大学大陆动力学国家重点实验室开放基金项目（DL2006001） |
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| 摘 要： | 根据古季风变化与生物生产总量之间的耦合关系,结合区域地质演变和地球卫星遥感影像解译成果,对引起高原内部古气候环境变化发展过程的启动激发因素和相互耦合机制及其驱动传递效应进行探索研究,这个方向目前仍然属于高原地质环境演变及全球变化的前沿领域。
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| 关 键 词： | 第四纪地质环境演化 地质构造事件响应 地球场效动力传递链 青藏高原腹地 |
| 收稿时间： | 2008-01-02 |
| 修稿时间： | 2008-06-02 |
The earth dynamical mechanism for the geological environmental evolution of quaternary period in the hinterland area of Qinghai-Xizang (Tibet) Plateau |
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| Hu Dongsheng and Zhang Guowei. The earth dynamical mechanism for the geological environmental evolution of quaternary period in the hinterland area of Qinghai-Xizang (Tibet) Plateau[J]. Engineering Sciences, 2011, 9(1): 81-88 |
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| Authors: | Hu Dongsheng and Zhang Guowei |
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| Affiliation: | College of Resources Environment Sciences, Hunan Normal University, Changsha |
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| Abstract: | Based on the coupling relation between the ancient monsoon change and the biologic produce gross, combining with the develop process of region geologic evolvement and the disabuse products of earth satellite remote sensing images, the startup blaze factor and mutual coupling mechanism and its drive transfer effect that caused the ancient climatic environment change in the plateau internal area were researched, This direction now still belong to frontier field in the evolvement of plateau geologic environment and its global change. |
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| Keywords: | geological environment evolvement of Quaternary respond of geologic structural events motive deliver chain of the earth field effect hinterland area of the Qinghai- Xizang (Tibet) Plateau |
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