INTRAPLATE THRUST EARTHQUAKE IN THE SOUTH CHINA SEA

被引:20
作者
WANG, SC [1 ]
GELLER, RJ [1 ]
STEIN, S [1 ]
TAYLOR, B [1 ]
机构
[1] COLUMBIA UNIV,LAMONT DOHERTY GEOL OBSERV,PALISADES,NY 10964
来源
JOURNAL OF GEOPHYSICAL RESEARCH | 1979年 / 84卷 / NB10期
关键词
D O I
10.1029/JB084iB10p05627
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
To investigate the state of stress in marginal seas, we have studied the October 7, 1965 (mb = 5.9, MS = 5.6), earthquake in the center of the South China Sea. This is one of the largest events in the interior of a marginal sea since the installation of the World-Wide Standard Seismograph Network. Using body and surface wave analysis, the focal mechanism is found to be almost pure thrust faulting at a very shallow depth (about 5km) with a seismic moment of 1 x 1025 dyn cm. The mechanism indicates horizontal compression oriented N38oE. Since this event does not occur on a bathymetric feature, its mechanism may indicate the overall state of stress in the South China Sea.-Authors
引用
收藏
页码:5627 / 5631
页数:5
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