Pervasive subduction zone devolatilization recycles CO2 into the forearc

The fate of subducted CO2 remains debated, with estimates mainly from numerical predictions varying from wholesale decarbonation of the shallow subducting slab to massive deep subduction of CO2. Here, the authors present field-based data and show that ~40% to ~65% of the CO2 in subducting crust is r...

Descripción completa

Guardado en:

Detalles Bibliográficos
Autores principales:	E. M. Stewart, Jay J. Ague
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2020
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/e61a2d7a36b4427e9c5a0fd393c601ea
Etiquetas:	Agregar Etiqueta Sin Etiquetas, Sea el primero en etiquetar este registro!

id	oai:doaj.org-article:e61a2d7a36b4427e9c5a0fd393c601ea
record_format	dspace
spelling	oai:doaj.org-article:e61a2d7a36b4427e9c5a0fd393c601ea2021-12-02T16:56:49ZPervasive subduction zone devolatilization recycles CO2 into the forearc10.1038/s41467-020-19993-22041-1723https://doaj.org/article/e61a2d7a36b4427e9c5a0fd393c601ea2020-12-01T00:00:00Zhttps://doi.org/10.1038/s41467-020-19993-2https://doaj.org/toc/2041-1723The fate of subducted CO2 remains debated, with estimates mainly from numerical predictions varying from wholesale decarbonation of the shallow subducting slab to massive deep subduction of CO2. Here, the authors present field-based data and show that ~40% to ~65% of the CO2 in subducting crust is released via metamorphic decarbonation reactions at forearc depths.E. M. StewartJay J. AgueNature PortfolioarticleScienceQENNature Communications, Vol 11, Iss 1, Pp 1-8 (2020)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q E. M. Stewart Jay J. Ague Pervasive subduction zone devolatilization recycles CO2 into the forearc
description	The fate of subducted CO2 remains debated, with estimates mainly from numerical predictions varying from wholesale decarbonation of the shallow subducting slab to massive deep subduction of CO2. Here, the authors present field-based data and show that ~40% to ~65% of the CO2 in subducting crust is released via metamorphic decarbonation reactions at forearc depths.
format	article
author	E. M. Stewart Jay J. Ague
author_facet	E. M. Stewart Jay J. Ague
author_sort	E. M. Stewart
title	Pervasive subduction zone devolatilization recycles CO2 into the forearc
title_short	Pervasive subduction zone devolatilization recycles CO2 into the forearc
title_full	Pervasive subduction zone devolatilization recycles CO2 into the forearc
title_fullStr	Pervasive subduction zone devolatilization recycles CO2 into the forearc
title_full_unstemmed	Pervasive subduction zone devolatilization recycles CO2 into the forearc
title_sort	pervasive subduction zone devolatilization recycles co2 into the forearc
publisher	Nature Portfolio
publishDate	2020
url	https://doaj.org/article/e61a2d7a36b4427e9c5a0fd393c601ea
work_keys_str_mv	AT emstewart pervasivesubductionzonedevolatilizationrecyclesco2intotheforearc AT jayjague pervasivesubductionzonedevolatilizationrecyclesco2intotheforearc
_version_	1718382712921784320

Pervasive subduction zone devolatilization recycles CO2 into the forearc

Ejemplares similares