• 责任者：Fang Ying (Institute of Earthquake Science ; China Earthquake Administration ; Beijing 100036 ; China) Jiang Zaisen
• 刊名：Earth Science
• 出版年：2009
• 卷期：34(3)
• 关键词：地壳运动 ; crustal movement ; 青藏高原 ; Qinghai-Tibetan Plateau
• 页码：p.399-404
• 图表：4 illus., 21 refs.
• 分类号：0300
• issnNo：ISSN1000-2383
• isbnNo：CN42-1233/P

Characteristics of current crustal movement in Qinghai-Tibetan Plateau were analyzed with least square collusion and wavelet using GPS data, and crustal movement strength and vortex movement were analyzed quantitatively. The conclusions are drawn as follows: The crustal movement strength in Qinghai-Tibetan Plateau decreases from west to east along arc tectonic ruptures formed by Kala-Kunlun, Mani, Yushu, Xianshuihe and Xiaojiang faults. The crustal movement strengths in north and west are stronger than those of south and east in the Sichuan-Yunnan block, of which east boundaries are obvious, and west boundaries are not.