Pliocene-Quaternary crustal melting in central and northern Tibet and insights into crustal flow

The role of the low velocity-high conductivity zones (LV–HCZs) in developing the Tibetan Plateau has remained controversial. Here, Wang et al.present new geochemical and petrological data that show the LV–HCZs are sources of partial melt thus giving insight into the development of the Tibetan Platea...

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Autores principales:	Qiang Wang, Chris J. Hawkesworth, Derek Wyman, Sun-Lin Chung, Fu-Yuan Wu, Xian-Hua Li, Zheng-Xiang Li, Guo-Ning Gou, Xiu-Zheng Zhang, Gong-Jian Tang, Wei Dan, Lin Ma, Yan-Hui Dong
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2016
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/73d278f1984c4e5f9987bfcdfc237105
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id	oai:doaj.org-article:73d278f1984c4e5f9987bfcdfc237105
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spelling	oai:doaj.org-article:73d278f1984c4e5f9987bfcdfc2371052021-12-02T14:38:34ZPliocene-Quaternary crustal melting in central and northern Tibet and insights into crustal flow10.1038/ncomms118882041-1723https://doaj.org/article/73d278f1984c4e5f9987bfcdfc2371052016-06-01T00:00:00Zhttps://doi.org/10.1038/ncomms11888https://doaj.org/toc/2041-1723The role of the low velocity-high conductivity zones (LV–HCZs) in developing the Tibetan Plateau has remained controversial. Here, Wang et al.present new geochemical and petrological data that show the LV–HCZs are sources of partial melt thus giving insight into the development of the Tibetan Plateau.Qiang WangChris J. HawkesworthDerek WymanSun-Lin ChungFu-Yuan WuXian-Hua LiZheng-Xiang LiGuo-Ning GouXiu-Zheng ZhangGong-Jian TangWei DanLin MaYan-Hui DongNature PortfolioarticleScienceQENNature Communications, Vol 7, Iss 1, Pp 1-11 (2016)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Qiang Wang Chris J. Hawkesworth Derek Wyman Sun-Lin Chung Fu-Yuan Wu Xian-Hua Li Zheng-Xiang Li Guo-Ning Gou Xiu-Zheng Zhang Gong-Jian Tang Wei Dan Lin Ma Yan-Hui Dong Pliocene-Quaternary crustal melting in central and northern Tibet and insights into crustal flow
description	The role of the low velocity-high conductivity zones (LV–HCZs) in developing the Tibetan Plateau has remained controversial. Here, Wang et al.present new geochemical and petrological data that show the LV–HCZs are sources of partial melt thus giving insight into the development of the Tibetan Plateau.
format	article
author	Qiang Wang Chris J. Hawkesworth Derek Wyman Sun-Lin Chung Fu-Yuan Wu Xian-Hua Li Zheng-Xiang Li Guo-Ning Gou Xiu-Zheng Zhang Gong-Jian Tang Wei Dan Lin Ma Yan-Hui Dong
author_facet	Qiang Wang Chris J. Hawkesworth Derek Wyman Sun-Lin Chung Fu-Yuan Wu Xian-Hua Li Zheng-Xiang Li Guo-Ning Gou Xiu-Zheng Zhang Gong-Jian Tang Wei Dan Lin Ma Yan-Hui Dong
author_sort	Qiang Wang
title	Pliocene-Quaternary crustal melting in central and northern Tibet and insights into crustal flow
title_short	Pliocene-Quaternary crustal melting in central and northern Tibet and insights into crustal flow
title_full	Pliocene-Quaternary crustal melting in central and northern Tibet and insights into crustal flow
title_fullStr	Pliocene-Quaternary crustal melting in central and northern Tibet and insights into crustal flow
title_full_unstemmed	Pliocene-Quaternary crustal melting in central and northern Tibet and insights into crustal flow
title_sort	pliocene-quaternary crustal melting in central and northern tibet and insights into crustal flow
publisher	Nature Portfolio
publishDate	2016
url	https://doaj.org/article/73d278f1984c4e5f9987bfcdfc237105
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Pliocene-Quaternary crustal melting in central and northern Tibet and insights into crustal flow

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