中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Eocene Neotethyan slab breakoff in southern Tibet inferred from the Linzizong volcanic record

文献类型:期刊论文

作者Lee, Hao-Yang1; Chung, Sun-Lin1; Lo, Ching-Hua1; Ji, Jianqing2; Lee, Tung-Yi3; Qian, Qing4; Zhang, Qi4
刊名TECTONOPHYSICS
出版日期2009-11-01
卷号477期号:1-2页码:20-35
关键词Linzizong volcanism Tibet Neotethyan subduction Slab breakoff India-Asia collision
ISSN号0040-1951
DOI10.1016/j.tecto.2009.02.031
文献子类Article
英文摘要Formation of the Linzizong volcanic successions in the Lhasa terrane, southern Tibet has long been related to northward subduction of the Neotethyan oceanic slab under Asia. Here we report new (40)Ar/(39)Ar age results for the volcanic rocks recovered from a large area (29 degrees N to 32 degrees N and 85 degrees E to 93 degrees E) that, together with literature data, delineate two discrete stages of volcanism. These are a widespread Cretaceous stage and an intense, but spatially confined, Paleogene stage. The latter, occurring only in the southern part of the Lhasa terrane, resulted in the Linzizong volcanic successions. Our data, furthermore, suggest southward migration and intensification of the volcanism in the Lhasa terrane with magmatic "flare-ups" at ca. 50 Ma. While the volcanic successions consist dominantly of calc-alkaline rocks typical of arc lava geochemistry, those formed during the flare-up period show significant compositional variations from low-K tholeiitic through calc-alkaline to shoshonitic magma suites. These observations enable us to interpret the volcanic southward migration and following flare-ups as the consequences of rollback and breakoff of the subducted Neotethyan slab that occurred ahead and in the early stage, respectively. of the India-Asia collision. Our interpretation that involves a major Eocene tectonomagmatic activity, and concomitant topographic uplift, in southern Tibet is consistent with Himalayan metamorphic constraints, regional sedimentary records and seismic tomography. Crown Copyright (C) 2009 Published by Elsevier B.V. All rights reserved.
WOS关键词INDO-ASIAN COLLISION ; TECTONIC EVOLUTION ; POSTCOLLISIONAL MAGMATISM ; CONTINENTAL COLLISION ; CALC-ALKALINE ; SW TIBET ; SUBDUCTION ; BASIN ; DETACHMENT ; PLATEAU
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000271776600003
出版者ELSEVIER SCIENCE BV
资助机构National Science Council, Taiwan, ROC ; National Science Council, Taiwan, ROC ; National Science Council, Taiwan, ROC ; National Science Council, Taiwan, ROC ; National Science Council, Taiwan, ROC ; National Science Council, Taiwan, ROC ; National Science Council, Taiwan, ROC ; National Science Council, Taiwan, ROC
源URL[http://ir.iggcas.ac.cn/handle/132A11/71638]  
专题中国科学院地质与地球物理研究所
通讯作者Lee, Hao-Yang
作者单位1.Natl Taiwan Univ, Dept Geosci, Taipei 10617, Taiwan
2.Peking Univ, Sch Earth & Space Sci, Beijing 100871, Peoples R China
3.Natl Taiwan Normal Univ, Dept Earth Sci, Taipei, Taiwan
4.Chinese Acad Sci, Inst Geol & Geophys, Beijing, Peoples R China
推荐引用方式
GB/T 7714
Lee, Hao-Yang,Chung, Sun-Lin,Lo, Ching-Hua,et al. Eocene Neotethyan slab breakoff in southern Tibet inferred from the Linzizong volcanic record[J]. TECTONOPHYSICS,2009,477(1-2):20-35.
APA Lee, Hao-Yang.,Chung, Sun-Lin.,Lo, Ching-Hua.,Ji, Jianqing.,Lee, Tung-Yi.,...&Zhang, Qi.(2009).Eocene Neotethyan slab breakoff in southern Tibet inferred from the Linzizong volcanic record.TECTONOPHYSICS,477(1-2),20-35.
MLA Lee, Hao-Yang,et al."Eocene Neotethyan slab breakoff in southern Tibet inferred from the Linzizong volcanic record".TECTONOPHYSICS 477.1-2(2009):20-35.

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来源:地质与地球物理研究所

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