Lower-crustal earthquakes in southern Tibet are linked to eclogitization of dry metastable granulite

The triggering mechanism of deep seismicity in Tibet remains unclear. Here the authors use experiments to show that granulite when deformed becomes brittle as it passes into the ecologite stability field developing macroscopic riedel fault zones thus providing an explanation for deep seismicity in S...

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Autores principales:	Feng Shi, Yanbin Wang, Tony Yu, Lupei Zhu, Junfeng Zhang, Jianguo Wen, Julien Gasc, Sarah Incel, Alexandre Schubnel, Ziyu Li, Tao Chen, Wenlong Liu, Vitali Prakapenka, Zhenmin Jin
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2018
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/b0f67d21f85d4770a0817d87ab9880ff
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spelling	oai:doaj.org-article:b0f67d21f85d4770a0817d87ab9880ff2021-12-02T14:38:48ZLower-crustal earthquakes in southern Tibet are linked to eclogitization of dry metastable granulite10.1038/s41467-018-05964-12041-1723https://doaj.org/article/b0f67d21f85d4770a0817d87ab9880ff2018-08-01T00:00:00Zhttps://doi.org/10.1038/s41467-018-05964-1https://doaj.org/toc/2041-1723The triggering mechanism of deep seismicity in Tibet remains unclear. Here the authors use experiments to show that granulite when deformed becomes brittle as it passes into the ecologite stability field developing macroscopic riedel fault zones thus providing an explanation for deep seismicity in Southern Tibet.Feng ShiYanbin WangTony YuLupei ZhuJunfeng ZhangJianguo WenJulien GascSarah IncelAlexandre SchubnelZiyu LiTao ChenWenlong LiuVitali PrakapenkaZhenmin JinNature PortfolioarticleScienceQENNature Communications, Vol 9, Iss 1, Pp 1-13 (2018)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Feng Shi Yanbin Wang Tony Yu Lupei Zhu Junfeng Zhang Jianguo Wen Julien Gasc Sarah Incel Alexandre Schubnel Ziyu Li Tao Chen Wenlong Liu Vitali Prakapenka Zhenmin Jin Lower-crustal earthquakes in southern Tibet are linked to eclogitization of dry metastable granulite
description	The triggering mechanism of deep seismicity in Tibet remains unclear. Here the authors use experiments to show that granulite when deformed becomes brittle as it passes into the ecologite stability field developing macroscopic riedel fault zones thus providing an explanation for deep seismicity in Southern Tibet.
format	article
author	Feng Shi Yanbin Wang Tony Yu Lupei Zhu Junfeng Zhang Jianguo Wen Julien Gasc Sarah Incel Alexandre Schubnel Ziyu Li Tao Chen Wenlong Liu Vitali Prakapenka Zhenmin Jin
author_facet	Feng Shi Yanbin Wang Tony Yu Lupei Zhu Junfeng Zhang Jianguo Wen Julien Gasc Sarah Incel Alexandre Schubnel Ziyu Li Tao Chen Wenlong Liu Vitali Prakapenka Zhenmin Jin
author_sort	Feng Shi
title	Lower-crustal earthquakes in southern Tibet are linked to eclogitization of dry metastable granulite
title_short	Lower-crustal earthquakes in southern Tibet are linked to eclogitization of dry metastable granulite
title_full	Lower-crustal earthquakes in southern Tibet are linked to eclogitization of dry metastable granulite
title_fullStr	Lower-crustal earthquakes in southern Tibet are linked to eclogitization of dry metastable granulite
title_full_unstemmed	Lower-crustal earthquakes in southern Tibet are linked to eclogitization of dry metastable granulite
title_sort	lower-crustal earthquakes in southern tibet are linked to eclogitization of dry metastable granulite
publisher	Nature Portfolio
publishDate	2018
url	https://doaj.org/article/b0f67d21f85d4770a0817d87ab9880ff
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Lower-crustal earthquakes in southern Tibet are linked to eclogitization of dry metastable granulite

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