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DOI | 10.1016/j.epsl.2022.117974 |
Paleomagnetic constraint on the formation of the Eastern Himalayan Syntaxis: A new late Eocene result from the Mangkang area of the eastern Tibetan Plateau | |
Zhang, Zijian; Tong, Yabo; Jin, Shuchen; Sun, Xinxin; Hou, Lifu; Pei, Junling; Yang, Zhenyu | |
发表日期 | 2023 |
ISSN | 0012-821X |
EISSN | 1385-013X |
卷号 | 603 |
英文摘要 | The Eastern Himalayan Syntaxis (EHS) is a major structural and geomorphological unit in Eastern Tibet; however, its mechanism of formation and the extent of its northward effect of compression remain unclear. To address these questions, we conducted a paleomagnetic and geochronologic study of the late Eocene trachyte intrusive mass in the Mangkang area of Tibet. The U-Pb SHRIMP II age estimate of the trachyte intrusive mass is-40 Ma, and the estimated mean paleomagnetic direction we obtained is D=27.0 degrees, I=36.8 degrees, k=42.9, alpha 95=1.3 degrees, and n=282 specimens. These results indicate that the Mangkang area was located at a paleolatitude of 20.5 +/- 0.9 degrees N during the late Eocene. A comparison of paleolatitudes of the Qiangtang block with those inferred from the apparent polar wander paths (APWP) of India and Eurasia suggests that the Eastern Himalayan Syntaxis was formed after 35 Ma when Eurasia was penetrated by-600 km by northward-moving India. This is consistent with geologic evidence of intra-continental shortening in the foreland of the Eastern Himalayan syntaxis. The northward counterclockwise penetration of the corner of India also resulted in the large right-lateral strike-slip system of the Sagaing fault (SGF), with -400-600 km of displacement between the EHS and the Shan-Thai block. Thus, the northward wedging of the EHS indicates minimal southward displacement of the Shan-Thai block. Our results link the tectonic activity of the EHS to the lateral extrusion of the southeastern margin of the Tibetan Plateau, providing a new perspective on the evolution of this region since the late Eocene.(c) 2022 Elsevier B.V. All rights reserved. |
关键词 | Eastern Himalayan SyntaxisPaleomagnetismlate Eocenesoutheastern Tibetan Plateau |
英文关键词 | CLOCKWISE ROTATIONS; VOLCANIC-ROCKS; MAGNETIC-FIELD; INDO-CHINA; RED-BEDS; DEFORMATION; BLOCK; YUNNAN; ASIA; GEOCHRONOLOGY |
WOS研究方向 | Geochemistry & Geophysics |
WOS记录号 | WOS:000960609600001 |
来源期刊 | EARTH AND PLANETARY SCIENCE LETTERS |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/283623 |
作者单位 | Capital Normal University; China Geological Survey; Chinese Academy of Geological Sciences; Institute of Geomechanics, Chinese Academy of Geological Sciences |
推荐引用方式 GB/T 7714 | Zhang, Zijian,Tong, Yabo,Jin, Shuchen,et al. Paleomagnetic constraint on the formation of the Eastern Himalayan Syntaxis: A new late Eocene result from the Mangkang area of the eastern Tibetan Plateau[J],2023,603. |
APA | Zhang, Zijian.,Tong, Yabo.,Jin, Shuchen.,Sun, Xinxin.,Hou, Lifu.,...&Yang, Zhenyu.(2023).Paleomagnetic constraint on the formation of the Eastern Himalayan Syntaxis: A new late Eocene result from the Mangkang area of the eastern Tibetan Plateau.EARTH AND PLANETARY SCIENCE LETTERS,603. |
MLA | Zhang, Zijian,et al."Paleomagnetic constraint on the formation of the Eastern Himalayan Syntaxis: A new late Eocene result from the Mangkang area of the eastern Tibetan Plateau".EARTH AND PLANETARY SCIENCE LETTERS 603(2023). |
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