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DOI | 10.1029/2019GL086650 |
Pre-Oxfordian (>163 Ma) Ophiolite Obduction in Central Tibet | |
Ma A.; Hu X.; Kapp P.; BouDagher-Fadel M.; Lai W. | |
发表日期 | 2020 |
ISSN | 0094-8276 |
卷号 | 47期号:10 |
英文摘要 | The timing of Bangong-Nujiang suture ophiolite obduction between the Lhasa and Qiangtang terranes in central Tibet is important for understanding the closure history of the Meso-Tethys but remains poorly constrained. We investigated subaerial to shallow marine strata of the Dongqiao Formation that sit unconformably on Bangong-Nujiang suture ophiolites that crystallized in a supra-subduction zone setting at 189–181 Ma. Based on foraminiferal and coral studies, the depositional age of the Dongqiao Formation is constrained to be Oxfordian and Kimmeridgian (Late Jurassic). Provenance analyses including detrital modes, geochemistry of detrital chromian spinels, and U-Pb age populations of detrital zircons suggest the Dongqiao Formation was sourced from uplifted Bangong-Nujiang suture ophiolites and sedimentary and metamorphic rocks of Lhasa terrane affinity to the south. We conclude that Bangong-Nujiang suture ophiolites were obducted soon after crystallization (prior to Oxfordian time; >163 Ma) onto the Lhasa terrane or a microcontinent of Lhasa terrane affinity. ©2020. American Geophysical Union. All Rights Reserved. |
英文关键词 | Binary alloys; Metamorphic rocks; Sedimentary rocks; Uranium alloys; Bangong-Nujiang Suture; Detrital chromian spinel; Detrital modes; Detrital zircon; Provenance analysis; Qiangtang terrane; Shallow marine; Subduction zones; Lead alloys; foraminifera; geochemistry; Kimmeridgian; metamorphic rock; obduction; ophiolite; terrane; China; Lhasa Terrane; Xizang; Anthozoa |
语种 | 英语 |
来源期刊 | Geophysical Research Letters |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/170345 |
作者单位 | State Key Laboratory of Mineral Deposit Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing, China; Department of Geosciences, University of Arizona, Tucson, AZ, United States; Department of Earth Sciences, University College London, London, United Kingdom |
推荐引用方式 GB/T 7714 | Ma A.,Hu X.,Kapp P.,et al. Pre-Oxfordian (>163 Ma) Ophiolite Obduction in Central Tibet[J],2020,47(10). |
APA | Ma A.,Hu X.,Kapp P.,BouDagher-Fadel M.,&Lai W..(2020).Pre-Oxfordian (>163 Ma) Ophiolite Obduction in Central Tibet.Geophysical Research Letters,47(10). |
MLA | Ma A.,et al."Pre-Oxfordian (>163 Ma) Ophiolite Obduction in Central Tibet".Geophysical Research Letters 47.10(2020). |
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