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DOI10.1007/s11589-012-0870-2
Focal depth estimates of earthquakes in the Himalayan-Tibetan region from teleseismic waveform modeling
Bai, Ling; Ritsema, Jeroen; Zhao, Junmeng
通讯作者Bai, L (通讯作者)
发表日期2012
ISSN1674-4519
EISSN1867-8777
起始页码459
结束页码468
卷号25期号:5-6
英文摘要We estimate the focal depths and fault plane solutions of 46 moderate earthquakes in the Himalayan-Tibetan region by modeling the broadband waveforms of teleseismic P waves. The depths of 38 of these earthquakes range between 0-40 km, with a peak at similar to 5 km. One earthquake is located within the lower crust of the Indian shield. The remaining eight earthquakes occurred between depths of 80-120 km and are all located in the Pamir-Hindu Kush and the Indo-Myanmar deep seismic zones. None of the earthquakes outside these deep seismic zones are located in the mantle. Global centroid moment tensor (CMT) solutions indicate that most earthquakes in northern Tibet and northern India had thrust-faulting mechanisms and that normal and strike-slip faulting earthquakes occurred primarily in central Tibet. These mechanisms are consistent with the predominantly NNW-SSE compression in the direction of current Himalayan-Tibetan continental collision.
关键词UPPER-MANTLEVELOCITY STRUCTURESOUTHERN TIBETKII PENINSULATRAVEL-TIMESBENEATHINDIALITHOSPHERESTRENGTHDEFORMATION
英文关键词continental collision zone; Tibetan plateau; focal depth; strength of the continental lithosphere
语种英语
WOS研究方向Geochemistry & Geophysics
WOS类目Geochemistry & Geophysics
WOS记录号WOS:000210058700010
来源期刊EARTHQUAKE SCIENCE
来源机构中国科学院青藏高原研究所
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/258024
推荐引用方式
GB/T 7714
Bai, Ling,Ritsema, Jeroen,Zhao, Junmeng. Focal depth estimates of earthquakes in the Himalayan-Tibetan region from teleseismic waveform modeling[J]. 中国科学院青藏高原研究所,2012,25(5-6).
APA Bai, Ling,Ritsema, Jeroen,&Zhao, Junmeng.(2012).Focal depth estimates of earthquakes in the Himalayan-Tibetan region from teleseismic waveform modeling.EARTHQUAKE SCIENCE,25(5-6).
MLA Bai, Ling,et al."Focal depth estimates of earthquakes in the Himalayan-Tibetan region from teleseismic waveform modeling".EARTHQUAKE SCIENCE 25.5-6(2012).
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