• 责任者：Jiang Kezhi (College of Geophysical ; Chengdu University of Technology ; Chengdu 610059 ; China) ; Zhu Jieshou
• 刊名：North China Earthquake Sciences
• 出版年：2012
• 卷期：30(2)
• 关键词：面波 ; surface waves ; 岩石圈 ; lithosphere ; 欧亚板块 ; Eurasian Plate
• 页码：p.1-7
• 图表：3 illus., 13 refs.
• 分类号：0400
• issnNo：ISSN1003-1375
• isbnNo：CN13-1102/P

///This paper deals with the high resolution surface wave tomography in Eurasia and its surrounding seas (20°W～160°E, 20°S～80°N). The results show that in Eurasia and its surrounding seas, the lithosphere thickness is from 40～60 km (continental rift zone) to 190～220 km (Craton region), the lithosphere velocity range is 4.30～4.80 km/s. Until 400 km depth, the various differences between the horizontal plate and block gradually decrease. In precambrian craton and block, the lithosphere is very thick and high V_S, the asthenosphere is very thin or non-existent. In marginal sea and Phanerozoic orogenic regional, lithosphere is thin and low V_S, the asthenosphere is very large. Distinctive features of oceanic plates is uncommonly high V_S in lithosphere, and abnormally low V_S in asthenosphere, the rate of mutation is very sharp in velocity-depth curves.