Detection of southward intracontinental subduction of Tibetan;lithosphere along the Bangong-Nujiang suture by P-to-S converted waves | |
Shi, D8; Zhao, WJ; Brown, L; Nelson, D; Zhao, X; Kind, R; Ni, J; Xiong, JY; Mechie, J; Guo, J | |
刊名 | GEOLOGY
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2004 | |
卷号 | 32期号:3页码:209-212 |
关键词 | receiver function lithospheric structure continental collision Tibetan Plateau |
ISSN号 | 0091-7613 |
DOI | 10.1130/G19814.1 |
英文摘要 | Teleseismic primary (P) to secondary (S) converted waves recorded on the INDEPTH III seismic array have been used to detect lithospheric-scale deformation structures of the central Tibetan Plateau from the central Lhasa terrane to the central Qiangtang terrane. A south-dipping crustal converter is seen from the upper crust near the 500-km-long metamorphic core complex exposures in the Qiangtang terrane to the lower crust near the Bangong-NuJiang suture. At deeper depths, a southeast-dipping mantle converter is seen extending from similar to50 km north of the Bangong-Nujiang suture at the depth of the Moho, to a depth of similar to180 km, similar to100 km south of the Bangong-Nujiang suture. We found the observations to be most consistent with a model of lithospheric deformation involving (1) southward subduction of the Tibetan lithospheric mantle along the Bangong-Nujiang suture and (2) thickening of the central Tibetan crust through a thick-skinned, crustal accretionary thrust-wedge structure in response to the India's collision with Asia. |
学科主题 | 构造地质学 |
WOS关键词 | MANTLE BENEATH TIBET ; SOUTHERN TIBET ; ANISOTROPY BENEATH ; CRUSTAL ; STRUCTURE ; NORTHERN TIBET ; PLATEAU ; EVOLUTION ; BLOCK ; FLOW |
WOS研究方向 | Geology |
语种 | 英语 |
出版者 | GEOLOGICAL SOC AMERICA, INC |
WOS记录号 | WOS:000189284200009 |
内容类型 | 期刊论文 |
源URL | [http://119.78.100.197/handle/2HKVOGP0/37678] ![]() |
专题 | 中国地质科学院 |
作者单位 | 1.Chinese Acad Geol Sci, Inst Mineral Resources, Beijing 100037, Peoples R China. 2.China Univ Geosci, Beijing 100083, Peoples R China. 3.Cornell Univ, Dept Geol Sci, Ithaca, NY 14853 USA. 4.Syracuse Univ, Dept Earth Sci, Syracuse, NY 13244 USA. 5.Geoforschungszentrum Potsdam, D-14473 Potsdam, Germany. 6.New Mexico State Univ, Dept Phys, Las Cruces, NM 88003 USA. 7.Stanford Univ, Dept Geophys, Stanford, CA 94305 USA. 8.中国地质科学院矿产资源研究所 |
推荐引用方式 GB/T 7714 | Shi, D,Zhao, WJ,Brown, L,et al. Detection of southward intracontinental subduction of Tibetan;lithosphere along the Bangong-Nujiang suture by P-to-S converted waves[J]. GEOLOGY,2004,32(3):209-212. |
APA | Shi, D.,Zhao, WJ.,Brown, L.,Nelson, D.,Zhao, X.,...&Hearn, T.(2004).Detection of southward intracontinental subduction of Tibetan;lithosphere along the Bangong-Nujiang suture by P-to-S converted waves.GEOLOGY,32(3),209-212. |
MLA | Shi, D,et al."Detection of southward intracontinental subduction of Tibetan;lithosphere along the Bangong-Nujiang suture by P-to-S converted waves".GEOLOGY 32.3(2004):209-212. |
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