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DOI | 10.1016/j.tecto.2020.228661 |
Response of Yunnan crustal structure to eastward growth of the Tibet Plateau and subduction of the India plate in Cenozoic | |
Ling Y.; Zheng T.; He Y.; Hou G. | |
发表日期 | 2020 |
ISSN | 00401951 |
卷号 | 797 |
英文摘要 | Most previous studies advocate that crustal weakening in the Yunnan area is predominantly the result of eastward growth of the Tibetan Plateau. Here we observe regional variations in the Yunnan crustal structure from the waveform characteristic variations of receiver functions at 342 seismic stations. Furthermore, receiver function imaging along three seismic sections reveals the response of crustal structure to different tectonic evolution. Our results show that northwestern Yunnan is characterized by 49–64 km-thick crust with multi-layer low-velocity materials and local lower crustal “doublet”. These low-velocity structures may reflect partial melting caused by crustal thickening associated with the eastward growth of the plateau. However, in southern and eastern parts of Yunnan, the topography of the Moho varies relatively gently with crustal thicknesses of 26–42 km, and widespread low-velocity zones are located above the crust-mantle boundary. We speculate that these features might favor the action of partial melting of crust triggered by asthenospheric upwelling related to the subduction of the India plate. © 2020 Elsevier B.V. |
关键词 | Asthenospheric upwellingCrustal structureEastward growth of the Tibetan PlateauReceiver functionsYunnan Province |
英文关键词 | Melting; Seismology; Structural geology; Topography; Crustal structure; Crustal thickenings; Low velocity zones; Northwestern Yunnan; Receiver functions; Regional variation; Tectonic evolution; Waveform characteristics; Plates (structural components); crustal structure; crustal thickening; growth response; Indian plate; Moho; plate motion; plate tectonics; subduction zone; tectonic evolution; tectonic setting; China; Xizang; Yunnan |
语种 | 英语 |
来源期刊 | Tectonophysics |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/207811 |
作者单位 | Key Laboratory of Earth and Planetary Physics, Institute of Geology and Geophysics, Chinese Academy of Sciences (CAS), Beijing, 100029, China; Innovation Academy for Earth Science, CAS, Beijing, 10029, China; CAS Center for Excellence in Tibetan Plateau Earth Sciences, CAS, Beijing, 100101, China |
推荐引用方式 GB/T 7714 | Ling Y.,Zheng T.,He Y.,et al. Response of Yunnan crustal structure to eastward growth of the Tibet Plateau and subduction of the India plate in Cenozoic[J],2020,797. |
APA | Ling Y.,Zheng T.,He Y.,&Hou G..(2020).Response of Yunnan crustal structure to eastward growth of the Tibet Plateau and subduction of the India plate in Cenozoic.Tectonophysics,797. |
MLA | Ling Y.,et al."Response of Yunnan crustal structure to eastward growth of the Tibet Plateau and subduction of the India plate in Cenozoic".Tectonophysics 797(2020). |
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