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DOI10.1111/j.1365-246X.2011.05154.x
The lithosphere-asthenosphere boundary revealed by S-receiver functions from the Hi-CLIMB experiment
Xu, Qiang; Zhao, Junmeng; Pei, Shunping; Liu, Hongbing
通讯作者Xu, Q (通讯作者)
发表日期2011
ISSN0956-540X
起始页码414
结束页码420
卷号187期号:1
英文摘要Detailed high-resolution images of the crust-mantle and lithosphere-asthenosphere boundaries (the Moho and the LAB, respectively) have been well observed by applying an S-receiver function technique to data collected by the Hi-CLIMB (Himalayan-Tibetan Continental Lithosphere During Mountain Building) experiment. The Moho depth variation in the range of similar to 50-70 km is in good agreement with that from previous P-receiver function results. The significant variation in the LAB depth indicates that the subducting Indian lithosphere drops northwards from a depth of similar to 80 km beneath the Himalayas to similar to 130 km just north of the Bangong-Nujiang suture at similar to 33.0 degrees N, and undergoes a transition from low angle to flat subduction beneath the Yarlung-Zangbo suture. Our findings provide new seismic constraints on the 3-D subducting configuration of the Indian lithosphere beneath Tibet.
关键词TIBET COLLISION ZONEMANTLE BENEATH TIBETSOUTHERN TIBETANISOTROPY BENEATHCRUSTAL STRUCTURESEISMIC EVIDENCEPLATEAUSUBDUCTIONEVOLUTIONHIMALAYA
英文关键词Body waves; Dynamics of lithosphere and mantle; Asia
语种英语
WOS研究方向Geochemistry & Geophysics
WOS类目Geochemistry & Geophysics
WOS记录号WOS:000295015100029
来源期刊GEOPHYSICAL JOURNAL INTERNATIONAL
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/257843
推荐引用方式
GB/T 7714
Xu, Qiang,Zhao, Junmeng,Pei, Shunping,et al. The lithosphere-asthenosphere boundary revealed by S-receiver functions from the Hi-CLIMB experiment[J]. 中国科学院青藏高原研究所,2011,187(1).
APA Xu, Qiang,Zhao, Junmeng,Pei, Shunping,&Liu, Hongbing.(2011).The lithosphere-asthenosphere boundary revealed by S-receiver functions from the Hi-CLIMB experiment.GEOPHYSICAL JOURNAL INTERNATIONAL,187(1).
MLA Xu, Qiang,et al."The lithosphere-asthenosphere boundary revealed by S-receiver functions from the Hi-CLIMB experiment".GEOPHYSICAL JOURNAL INTERNATIONAL 187.1(2011).
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