青藏高原腹地第四纪地质环境演化的地球动力学机制
The earth dynamical mechanism for the geological environmental evolution of quaternary period in the hinterland area of Qinghai-Xizang (Tibet) Plateau
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。
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.
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
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
胡东生（1951―），男，甘肃天水市人，教授，主要从事资源环境和遥感地质学与地球动力学及全球变化等方面的研究
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