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DOI10.1016/j.lithos.2023.107044
Are low-velocity zones within the Tibetan crust the result of crustal melting from at least 28 Ma?
Zhang, Xiu-Zheng; Wang, Qiang; Wyman, Derek; Kerr, Andrew C.; Gou, Guo-Ning; Dan, Wei; Qi, Yue
发表日期2023
ISSN0024-4937
EISSN1872-6143
卷号440
英文摘要Geophysically identified low-velocity zones (LVZs) are widespread within the Tibetan lower-middle crust, but their nature and role in models of the development of the Tibetan Plateau remain controversial. The debate stems mainly from whether the Tibetan crust was hydrous and has therefore undergone substantial melting. Here, we identify hydrous crustal xenoliths incorporated into 28 Ma syenite porphyries from central-northern Tibet. These xenoliths indicate the former existence of a cold (T = 680-790 degrees C) and water-rich (1.10-1.50 wt%) crustal endmember at a depth of 14-40 km in the Tibetan lower-middle crust. Our new petrological evidence indicates the LVZs are partially molten layers that have existed within the Tibetan crust since at least 28 Ma. High- to ultrahigh-temperature metamorphism since the Miocene is inferred to have triggered widespread melting of the former hydrous crust, which would have promoted the development of LVZs and resulted in a flat Tibet.
关键词Crustal xenolithsLow-velocity zonesLower-middle crustCrustal meltingTibetan Plateau
英文关键词PLATEAU; CONSTRAINTS; TEMPERATURE; PALEOCENE; EXTRUSION; XENOLITHS; GRANITE; GENESIS; UPLIFT
WOS研究方向Geochemistry & Geophysics ; Mineralogy
WOS记录号WOS:000967994700001
来源期刊LITHOS
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/283583
作者单位Chinese Academy of Sciences; Guangzhou Institute of Geochemistry, CAS; University of Sydney; Cardiff University
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GB/T 7714
Zhang, Xiu-Zheng,Wang, Qiang,Wyman, Derek,et al. Are low-velocity zones within the Tibetan crust the result of crustal melting from at least 28 Ma?[J],2023,440.
APA Zhang, Xiu-Zheng.,Wang, Qiang.,Wyman, Derek.,Kerr, Andrew C..,Gou, Guo-Ning.,...&Qi, Yue.(2023).Are low-velocity zones within the Tibetan crust the result of crustal melting from at least 28 Ma?.LITHOS,440.
MLA Zhang, Xiu-Zheng,et al."Are low-velocity zones within the Tibetan crust the result of crustal melting from at least 28 Ma?".LITHOS 440(2023).
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