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《Acta Geologica Sinica》 1998-03
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The 3-d Deformational Movement Episodes and Neotectonic Domains in the Qinghai-Tibet Plateau

Ma Zongjin, Zhang Jiasheng and Wang Yipeng(Institute of Geology, State Seismological Bureau , Beijing, 100029 )  
The formation of the Qinghai-Tibet plateau has progressed through four partly overlapped tectonic episodes. The a episode mainly witnessed NS shortening and northward movement in 45 ~35 Ma. This was followed by a long period of slow uplift, i. e. ,the (3 episode,from 35 to 5. 3 Ma. The 7 episode was a short period of rapid uplift that started 5. 3 Ma ago and reached its culmination after 3. 0 Ma. The 6 episode was characterized by E-W extension. It occurred before 3. 0 Ma B P in the Himalaya area and spread to the whole plateau after 3. 0 Ma B P. Extension became a dominant mode of deformation movement in the Quaternary. On the basis of the inhomo-geneity of tectonic deformation in space and time in the γ and δepisodes,the Qinghai-Tibet is divided into three tectonic domains,Tibet ,Qingtang and Qaidam.
【Fund】: 国家攀登计划“现代地壳运动和地球动力学研究”;; 国家自然科学基金(编号49672155
【CateGory Index】: P542.2
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