Massive production of abiotic methane during subduction evidenced in metamorphosed ophicarbonates from the Italian Alps

Alteration of ultramafic rocks plays a role in hydrocarbon production, but little is known about this process at depth. Here, the authors provide evidence that alteration of carbonated ultramafic rocks at high-pressures are an important source of abiotic methanogenesis with implications for deep C m...

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Autores principales:	Alberto Vitale Brovarone, Isabelle Martinez, Agnès Elmaleh, Roberto Compagnoni, Carine Chaduteau, Cristiano Ferraris, Imène Esteve
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2017
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/aa9b61727d5245c4a88c42a9b0d2815b
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spelling	oai:doaj.org-article:aa9b61727d5245c4a88c42a9b0d2815b2021-12-02T14:42:41ZMassive production of abiotic methane during subduction evidenced in metamorphosed ophicarbonates from the Italian Alps10.1038/ncomms141342041-1723https://doaj.org/article/aa9b61727d5245c4a88c42a9b0d2815b2017-02-01T00:00:00Zhttps://doi.org/10.1038/ncomms14134https://doaj.org/toc/2041-1723Alteration of ultramafic rocks plays a role in hydrocarbon production, but little is known about this process at depth. Here, the authors provide evidence that alteration of carbonated ultramafic rocks at high-pressures are an important source of abiotic methanogenesis with implications for deep C mobility.Alberto Vitale BrovaroneIsabelle MartinezAgnès ElmalehRoberto CompagnoniCarine ChaduteauCristiano FerrarisImène EsteveNature PortfolioarticleScienceQENNature Communications, Vol 8, Iss 1, Pp 1-13 (2017)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Alberto Vitale Brovarone Isabelle Martinez Agnès Elmaleh Roberto Compagnoni Carine Chaduteau Cristiano Ferraris Imène Esteve Massive production of abiotic methane during subduction evidenced in metamorphosed ophicarbonates from the Italian Alps
description	Alteration of ultramafic rocks plays a role in hydrocarbon production, but little is known about this process at depth. Here, the authors provide evidence that alteration of carbonated ultramafic rocks at high-pressures are an important source of abiotic methanogenesis with implications for deep C mobility.
format	article
author	Alberto Vitale Brovarone Isabelle Martinez Agnès Elmaleh Roberto Compagnoni Carine Chaduteau Cristiano Ferraris Imène Esteve
author_facet	Alberto Vitale Brovarone Isabelle Martinez Agnès Elmaleh Roberto Compagnoni Carine Chaduteau Cristiano Ferraris Imène Esteve
author_sort	Alberto Vitale Brovarone
title	Massive production of abiotic methane during subduction evidenced in metamorphosed ophicarbonates from the Italian Alps
title_short	Massive production of abiotic methane during subduction evidenced in metamorphosed ophicarbonates from the Italian Alps
title_full	Massive production of abiotic methane during subduction evidenced in metamorphosed ophicarbonates from the Italian Alps
title_fullStr	Massive production of abiotic methane during subduction evidenced in metamorphosed ophicarbonates from the Italian Alps
title_full_unstemmed	Massive production of abiotic methane during subduction evidenced in metamorphosed ophicarbonates from the Italian Alps
title_sort	massive production of abiotic methane during subduction evidenced in metamorphosed ophicarbonates from the italian alps
publisher	Nature Portfolio
publishDate	2017
url	https://doaj.org/article/aa9b61727d5245c4a88c42a9b0d2815b
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Massive production of abiotic methane during subduction evidenced in metamorphosed ophicarbonates from the Italian Alps

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