地震学报（英文版）2001，Vol.14Issue(4)：384-393,10.
General characteristics of the recent hori-zontal crustal movement in Chinese main-land
General characteristics of the recent hori-zontal crustal movement in Chinese main-land
顾国华 1申旭辉 1王敏 2郑贵明 1方颖 1李鹏1
作者信息
- 1. Center for Analysis and Prediction, China Seismological Bureau,
- 2. First Crustal Deformation Monitoring Center, China Seismological Bureau,
- 折叠
摘要
Abstract
In this paper, the horizontal crustal movement obtained from GPS observations in 1998 and 2000 at basic and fidu-cial stations in the Crustal Movement Observation Network of China (CMONOC) is introduced. A brief introduc-tion of the field observations, the data processing with GAMIT/GLOBK software and the accuracy of the GPS observations is given. In average the accuracy of the results for each year is about 2 mm in the horizontal compo-nents and 5 mm in the vertical component, and the average accuracy of horizontal displacements at a station is about 3 mm. The results of crustal movement during the period from early September 1998 to mid June, 2000, including the displacements at each station with datum definition of a group of stable stations of insignificant rela-tive movements among themselves in the eastern part of China, strains in different parts of the network and rota-tions in some parts, are obtained. Based on the crustal movement maps which are more complete and detailed than previous ones, the general characteristics of the recent crustal movement in Chinese mainland are discussed. During the above mentioned period of observations, the crustal deformation in the eastern part of China was relatively small and quite stable. With reference to a group of stable stations with small relative movement in the eastern part of China, the northeastern China block moved northward for about 10 mm, the South China block moved south-eastward for about 9 mm. In reference to the eastern part the northwestern part of China moved northward for about 26 mm, the Tibetan area in southwestern part of China moved mainly northward for about 32 mm. The area in Yunnan and east Tibet showed significant clockwise tectonic rotation of 0.00452 or average rotational displace-ment of 12 mm with the rotation center at 26.5°N and 95.5°E. The North-South Seismic Belt in the middle part of China is of active and complicated deformation. The observation results show that the northward pushing by the Indian plate has still played the dominant role in the crustal movement in Chinese mainland.分类
天文与地球科学引用本文复制引用
顾国华,申旭辉,王敏,郑贵明,方颖,李鹏..General characteristics of the recent hori-zontal crustal movement in Chinese main-land[J].地震学报（英文版）,2001,14(4):384-393,10.
