Stagnant forearc mantle wedge inferred from mapping of shear-wave anisotropy using S-net seafloor seismometers

Knowledge of shear-wave anisotropy is important to understanding the structure and dynamics of the subduction zone mantle wedge. Here, the authors find unambiguous evidence that forearc anisotropy resides in the upper-plate crust, while weak anisotropy in the most seaward part of the mantle wedge in...

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Autores principales:	Naoki Uchida, Junichi Nakajima, Kelin Wang, Ryota Takagi, Keisuke Yoshida, Takashi Nakayama, Ryota Hino, Tomomi Okada, Youichi Asano
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2020
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/15217a8256a74a9fbd41c5af53b822e9
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id	oai:doaj.org-article:15217a8256a74a9fbd41c5af53b822e9
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spelling	oai:doaj.org-article:15217a8256a74a9fbd41c5af53b822e92021-12-02T15:39:28ZStagnant forearc mantle wedge inferred from mapping of shear-wave anisotropy using S-net seafloor seismometers10.1038/s41467-020-19541-y2041-1723https://doaj.org/article/15217a8256a74a9fbd41c5af53b822e92020-11-01T00:00:00Zhttps://doi.org/10.1038/s41467-020-19541-yhttps://doaj.org/toc/2041-1723Knowledge of shear-wave anisotropy is important to understanding the structure and dynamics of the subduction zone mantle wedge. Here, the authors find unambiguous evidence that forearc anisotropy resides in the upper-plate crust, while weak anisotropy in the most seaward part of the mantle wedge indicates decoupling from the slabNaoki UchidaJunichi NakajimaKelin WangRyota TakagiKeisuke YoshidaTakashi NakayamaRyota HinoTomomi OkadaYouichi AsanoNature PortfolioarticleScienceQENNature Communications, Vol 11, Iss 1, Pp 1-8 (2020)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Naoki Uchida Junichi Nakajima Kelin Wang Ryota Takagi Keisuke Yoshida Takashi Nakayama Ryota Hino Tomomi Okada Youichi Asano Stagnant forearc mantle wedge inferred from mapping of shear-wave anisotropy using S-net seafloor seismometers
description	Knowledge of shear-wave anisotropy is important to understanding the structure and dynamics of the subduction zone mantle wedge. Here, the authors find unambiguous evidence that forearc anisotropy resides in the upper-plate crust, while weak anisotropy in the most seaward part of the mantle wedge indicates decoupling from the slab
format	article
author	Naoki Uchida Junichi Nakajima Kelin Wang Ryota Takagi Keisuke Yoshida Takashi Nakayama Ryota Hino Tomomi Okada Youichi Asano
author_facet	Naoki Uchida Junichi Nakajima Kelin Wang Ryota Takagi Keisuke Yoshida Takashi Nakayama Ryota Hino Tomomi Okada Youichi Asano
author_sort	Naoki Uchida
title	Stagnant forearc mantle wedge inferred from mapping of shear-wave anisotropy using S-net seafloor seismometers
title_short	Stagnant forearc mantle wedge inferred from mapping of shear-wave anisotropy using S-net seafloor seismometers
title_full	Stagnant forearc mantle wedge inferred from mapping of shear-wave anisotropy using S-net seafloor seismometers
title_fullStr	Stagnant forearc mantle wedge inferred from mapping of shear-wave anisotropy using S-net seafloor seismometers
title_full_unstemmed	Stagnant forearc mantle wedge inferred from mapping of shear-wave anisotropy using S-net seafloor seismometers
title_sort	stagnant forearc mantle wedge inferred from mapping of shear-wave anisotropy using s-net seafloor seismometers
publisher	Nature Portfolio
publishDate	2020
url	https://doaj.org/article/15217a8256a74a9fbd41c5af53b822e9
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Stagnant forearc mantle wedge inferred from mapping of shear-wave anisotropy using S-net seafloor seismometers

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