中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Current-day tectonic motion and intraplate deformation-strain field obtained from space geodesy in the Pacific Plate

文献类型:期刊论文

作者Li Yan-Xing; Zhang Jing-Hua; He Jian-Kun; Li Jin-Ling; Li Zhi; Guo Liang-Qian; Zhang Zhong-Fu; Du Xue-Song
刊名CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION
出版日期2007-03-01
卷号50期号:2页码:437-447
关键词PCFC elastic motion equation two kinds of models intraplate deformation strain field
ISSN号0001-5733
文献子类Article
英文摘要In this paper we present a plate elastic motion equation, and based on the space geodetic data of the Pacific plate (PCFC), create an elastic motion model for the PCFC. The coincidence of this model with the plate real motion status is obviously better than that of the rigid motion model. Our research indicates that the angular velocity of the current-day rotation of the PCFC is 0.037 degrees/Ma larger than the average in the past 3 Ma. The horizontal deformation within the PCFC is evident. In the region to the north of 15 degrees S and to the west of ,204.5 degrees E, there exists a consistent west-trending deformation with the rates of 0.8 similar to 3.5 mm/a and 1.0 similar to 3.4 mm/a in the NW and SW directions, respectively. In the southeastern region of the plate, there exists a coincident east-trending deformation with the rates of 1.5 similar to 1.8 mm/a and 2.8 similar to 9.1 mm/a in the NE and SE directions, respectively. The spatial variation of horizontal strain field within the PCFC is regular. In the northwestern part of the PCFC, the principal compressive strain axis is NW - SE and the principal compressive strain rate is larger than the principal tensile strain rate; while in the southeastern part of the PCFC, the principal compressive strain axis is NE - SW and the principal tensile strain rate is larger than the principal compressive strain rate. The southeast boundary of the PCFC is a spreading one. The principal tensile strain rate near the boundary is the largest (average: 1.51 x 10(-9)/a) and the principal tensile strain axis is basically consistent with the extending direction of the oceanic ridge; the northwest boundary of the PCFC is an underthrusting one. The principal compressive strain rate near the boundary is the largest (average: 0.75 x 10(-9)/a) and the principal compressive strain axis is basically coincident with the underthrusting direction of the PCFC.
WOS关键词ITRF96 ; MODEL
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000245399900015
出版者SCIENCE CHINA PRESS
源URL[http://ir.iggcas.ac.cn/handle/132A11/68080]  
专题中国科学院地质与地球物理研究所
通讯作者Li Yan-Xing
作者单位1.China Earthquake Adm, Crust Monitoring & Applicat Ctr 1, Tianjin 300180, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
3.Chinese Acad Sci, Shanghai Astron Obser, Shanghai 200030, Peoples R China
4.Inst Equipment Technol & Command, Beijing 101416, Peoples R China
推荐引用方式
GB/T 7714
Li Yan-Xing,Zhang Jing-Hua,He Jian-Kun,et al. Current-day tectonic motion and intraplate deformation-strain field obtained from space geodesy in the Pacific Plate[J]. CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,2007,50(2):437-447.
APA Li Yan-Xing.,Zhang Jing-Hua.,He Jian-Kun.,Li Jin-Ling.,Li Zhi.,...&Du Xue-Song.(2007).Current-day tectonic motion and intraplate deformation-strain field obtained from space geodesy in the Pacific Plate.CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,50(2),437-447.
MLA Li Yan-Xing,et al."Current-day tectonic motion and intraplate deformation-strain field obtained from space geodesy in the Pacific Plate".CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION 50.2(2007):437-447.

入库方式: OAI收割

来源:地质与地球物理研究所

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