中国工程科学2011，Vol.13Issue(1)：81-88,8.
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
摘要
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.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/青藏高原腹地分类
天文与地球科学引用本文复制引用
胡东生,张华京,徐冰,温景春,田新红,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,2011,13(1):81-88,8.基金项目
中国可可西里地区国家重点科学考察项目(D2000204) （D2000204）
湖南省重点学科建设项目(D2007001) （D2007001）
西北大学大陆动力学国家重点实验室开放基金项目(DL2006001) （DL2006001）
