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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2017-02-01
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Series: | Nature Communications |
Online Access: | https://doi.org/10.1038/ncomms14134 |
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doaj-aa9b61727d5245c4a88c42a9b0d2815b2021-05-11T07:36:05ZengNature Publishing GroupNature Communications2041-17232017-02-018111310.1038/ncomms14134Massive production of abiotic methane during subduction evidenced in metamorphosed ophicarbonates from the Italian AlpsAlberto Vitale Brovarone0Isabelle Martinez1Agnès Elmaleh2Roberto Compagnoni3Carine Chaduteau4Cristiano Ferraris5Imène Esteve6Institut de Minéralogie, de Physique des Matériaux et de Cosmochimie UMR 7590 CNRS-UPMC-IRD-MNHNInstitut de Physique du Globe de Paris, Sorbonne Paris Cité, Université Paris Diderot, UMR 7154 CNRSInstitut de Minéralogie, de Physique des Matériaux et de Cosmochimie UMR 7590 CNRS-UPMC-IRD-MNHNDipartimento di Scienze della Terra, Università degli Studi di TorinoInstitut de Physique du Globe de Paris, Sorbonne Paris Cité, Université Paris Diderot, UMR 7154 CNRSInstitut de Minéralogie, de Physique des Matériaux et de Cosmochimie UMR 7590 CNRS-UPMC-IRD-MNHNInstitut de Minéralogie, de Physique des Matériaux et de Cosmochimie UMR 7590 CNRS-UPMC-IRD-MNHNAlteration 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.https://doi.org/10.1038/ncomms14134 |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Alberto Vitale Brovarone Isabelle Martinez Agnès Elmaleh Roberto Compagnoni Carine Chaduteau Cristiano Ferraris Imène Esteve |
spellingShingle |
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 Nature Communications |
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 Publishing Group |
series |
Nature Communications |
issn |
2041-1723 |
publishDate |
2017-02-01 |
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. |
url |
https://doi.org/10.1038/ncomms14134 |
work_keys_str_mv |
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