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引用本文:杨辉,王勇.?????????????????????????????????[J].大地测量与地球动力学,2007,27(2):25-31.
作者姓名:杨辉  王勇
作者单位:1. 中国科学院测量与地球物理研究所,武汉,430077;中国科学院研究生院,北京,100049
2. 中国科学院测量与地球物理研究所,武汉,430077
基金项目:中国科学院知识创新工程重要方向项目(KZCX2-YW-125),国家自然科学基金(40574033)
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文章编号:1671-5942(2007)02-0025-07
修稿时间:2006年8月31日

SIMULATION OF INFLUENCE OF LOWER-VELOCITY LAYER ON INTENSITY OF QINGHAI-TIBET PLATEAU LITHOSPHERE WITH 3D FINITE ELEMENT METHOD
Yang Hui,Wang Yong.SIMULATION OF INFLUENCE OF LOWER-VELOCITY LAYER ON INTENSITY OF QINGHAI-TIBET PLATEAU LITHOSPHERE WITH 3D FINITE ELEMENT METHOD[J].Journal of Geodesy and Geodynamics,2007,27(2):25-31.
Authors:Yang Hui  Wang Yong
Institution:1)Institute of Geodesy and Geophysics,CAS, Wuhan 4300772)Graduate School of the Chinese Academy of Science, Beijing 100049
Abstract:The downward deflection of the Qinghai-Tibet lithosphere due to the topographical load is calculated with finite element method by use of the 3D multilayered shell structural unit.Then,the influence of the lower-velocity layer of thermokarst on the intensity of the Qinghai-Tibet lithosphere in different regions is studied with multilayered mechanical model,based on the seismic-wave velocity structural model and the constrained Moho model.The results show that the lower-velocity layer of thermokarst has a stronger influence on the lithosphere in the eastern region of the Qinghai-Tibet plateau than that in the western region.
Keywords:Qinghai-Tibet plateau  lithosphere  FEM(Finte Element Method)  flexure  lower-velocity layer
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