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Volumn 325, Issue 5946, 2009, Pages 1371-1374

Underplating in the himalaya-tibet collision zone revealed by the Hi-CLIMB experiment

(31)  Nábělek, John a   Hetényi, György b,g   Vergne, Jérôme b,h   Sapkota, Soma c   Kafle, Basant c,i   Jiang, Mei d   Su, Heping d   Chen, John e   Huang, Bor Shouh f   Mitchell, L a   Sherstad, D a   Arsenault, M a   Baur, J a   Carpenter, S a   Donnahue, M a   Myers, D a   Tseng, T L j   Bardell, T j   Vanhoudnos, N j   Pandey, M c   more..


Author keywords

[No Author keywords available]

Indexed keywords

COLLISION ZONE; CRUST; CRUST-MANTLE BOUNDARY; EXPERIMENTAL STUDY; IMAGING METHOD; LITHOSPHERIC STRUCTURE; MOUNTAIN REGION; PLATE TECTONICS; SEISMIC DATA; SUBDUCTION; THRUST FAULT; UNDERPLATING; UPPER MANTLE;

EID: 70249104633     PISSN: 00368075     EISSN: 10959203     Source Type: Journal    
DOI: 10.1126/science.1167719     Document Type: Article
Times cited : (725)

References (34)
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    • The Hi-CLIMB network included 75 broadband seismic stations from the U.S. Program for Array Seismic Studies of the Continental Lithosphère (PASSCAL), supplemented in southern Tibet by 32 stations from Peking University and the Chinese Academy of Geological Sciences, PRC; and from the Academia Sinica, Taiwan. Throughout the experiment, the stations occupied 233 locations.
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    • note was supported by the French program DyETI. We acknowledge W.-P. Chen for the contribution to the planning of the experiment
    • The Hi-CLIMB team was supported by the U.S. NSF, Continental Dynamics Program, grant EAR 9909609. The fieldwork was also supported in part by the Department of Mines and Geology, Nepal; the Chinese Academy of Geological Sciences and Peking University; and the Institute of Earth Sciences, Academia Sinica, Taiwan. G.H.'s thesis (http://tel.archives-ouvertes.fr/tel-00194619/en/) was supported by the French program DyETI. We acknowledge W.-P. Chen for the contribution to the planning of the experiment.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.