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DOI | 10.1016/j.epsl.2008.06.038 |
Evidence for Early (> 44 Ma) Himalayan Crustal Thickening, Tethyan Himalaya, southeastern Tibet | |
Aikman, Amos B.; Harrison, T. Mark; Lin, Ding | |
通讯作者 | Harrison, TM (通讯作者) |
发表日期 | 2008 |
ISSN | 0012-821X |
EISSN | 1385-013X |
起始页码 | 14 |
结束页码 | 23 |
卷号 | 274期号:1-2 |
英文摘要 | Comprehensive understanding of Himalayan orogenesis is limited in part by a poor knowledge of the Eohimalayan episode; a phase of tectonic activity predating the better understood Neohimalayan crustal thickening associated with coaxial deformation along the Main Central thrust. The Cambo-Ordovician to Tertiary metasedimentary sequences outcropping within the Tethyan Himalaya are the structurally highest units of the Himalayan Fold and Thrust Belt; they and are inferred to have been the first to have accreted to Asia. A compilation of data from transects along the length of the main Himalayan arc shows that the Tethyan sequences have experienced at least five deformation events, although the timing of these episodes is poorly constrained. Emplacement of a series of undeformed granitoid bodies following the second of these events, which accounts for the majority of crustal thickening in the Tethyan Himalayan units, is constrained by U-Pb zircon dating to be older than 44.1 +/- 1.2 Ma. Thus, significant crustal thickening had occurred along the length of the proto-Himalayan arc by the mid-Eocene, or within 10 to 20 myr of the initiation of Himalayan orogenesis. (C) 2008 Elsevier ELV. All rights reserved. |
关键词 | FOLD-THRUST BELTU-PB AGESTECTONIC EVOLUTIONSTRUCTURAL EVOLUTIONSOUTHERN TIBETTERTIARY CONVERGENCECENTRAL NEPALKANGMAR DOMESUTURE ZONEHISTORY |
英文关键词 | Tethyan Himalaya; Tibet; U-Pb zircon; Dala granitoids |
语种 | 英语 |
WOS研究方向 | Geochemistry & Geophysics |
WOS类目 | Geochemistry & Geophysics |
WOS记录号 | WOS:000259912800002 |
来源期刊 | EARTH AND PLANETARY SCIENCE LETTERS |
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/257594 |
推荐引用方式 GB/T 7714 | Aikman, Amos B.,Harrison, T. Mark,Lin, Ding. Evidence for Early (> 44 Ma) Himalayan Crustal Thickening, Tethyan Himalaya, southeastern Tibet[J]. 中国科学院青藏高原研究所,2008,274(1-2). |
APA | Aikman, Amos B.,Harrison, T. Mark,&Lin, Ding.(2008).Evidence for Early (> 44 Ma) Himalayan Crustal Thickening, Tethyan Himalaya, southeastern Tibet.EARTH AND PLANETARY SCIENCE LETTERS,274(1-2). |
MLA | Aikman, Amos B.,et al."Evidence for Early (> 44 Ma) Himalayan Crustal Thickening, Tethyan Himalaya, southeastern Tibet".EARTH AND PLANETARY SCIENCE LETTERS 274.1-2(2008). |
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