Fluxing of mantle carbon as a physical agent for metallogenic fertilization of the crust

Magmatic systems play a crucial role in enriching the crust with volatiles and elements that reside primarily within the Earth’s mantle. Here, the authors show that carbon, as a buoyant supercritical CO2 fluid, could be a covert agent that may promote the physical transport of sulfides across the ma...

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Autores principales:	Daryl E. Blanks, David A. Holwell, Marco L. Fiorentini, Marilena Moroni, Andrea Giuliani, Santiago Tassara, José M. González-Jiménez, Adrian J. Boyce, Elena Ferrari
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2020
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/373a97b12f0b47f19fe150436d172881
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spelling	oai:doaj.org-article:373a97b12f0b47f19fe150436d1728812021-12-02T19:02:36ZFluxing of mantle carbon as a physical agent for metallogenic fertilization of the crust10.1038/s41467-020-18157-62041-1723https://doaj.org/article/373a97b12f0b47f19fe150436d1728812020-08-01T00:00:00Zhttps://doi.org/10.1038/s41467-020-18157-6https://doaj.org/toc/2041-1723Magmatic systems play a crucial role in enriching the crust with volatiles and elements that reside primarily within the Earth’s mantle. Here, the authors show that carbon, as a buoyant supercritical CO2 fluid, could be a covert agent that may promote the physical transport of sulfides across the mantle-crust transition.Daryl E. BlanksDavid A. HolwellMarco L. FiorentiniMarilena MoroniAndrea GiulianiSantiago TassaraJosé M. González-JiménezAdrian J. BoyceElena FerrariNature PortfolioarticleScienceQENNature Communications, Vol 11, Iss 1, Pp 1-11 (2020)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Daryl E. Blanks David A. Holwell Marco L. Fiorentini Marilena Moroni Andrea Giuliani Santiago Tassara José M. González-Jiménez Adrian J. Boyce Elena Ferrari Fluxing of mantle carbon as a physical agent for metallogenic fertilization of the crust
description	Magmatic systems play a crucial role in enriching the crust with volatiles and elements that reside primarily within the Earth’s mantle. Here, the authors show that carbon, as a buoyant supercritical CO2 fluid, could be a covert agent that may promote the physical transport of sulfides across the mantle-crust transition.
format	article
author	Daryl E. Blanks David A. Holwell Marco L. Fiorentini Marilena Moroni Andrea Giuliani Santiago Tassara José M. González-Jiménez Adrian J. Boyce Elena Ferrari
author_facet	Daryl E. Blanks David A. Holwell Marco L. Fiorentini Marilena Moroni Andrea Giuliani Santiago Tassara José M. González-Jiménez Adrian J. Boyce Elena Ferrari
author_sort	Daryl E. Blanks
title	Fluxing of mantle carbon as a physical agent for metallogenic fertilization of the crust
title_short	Fluxing of mantle carbon as a physical agent for metallogenic fertilization of the crust
title_full	Fluxing of mantle carbon as a physical agent for metallogenic fertilization of the crust
title_fullStr	Fluxing of mantle carbon as a physical agent for metallogenic fertilization of the crust
title_full_unstemmed	Fluxing of mantle carbon as a physical agent for metallogenic fertilization of the crust
title_sort	fluxing of mantle carbon as a physical agent for metallogenic fertilization of the crust
publisher	Nature Portfolio
publishDate	2020
url	https://doaj.org/article/373a97b12f0b47f19fe150436d172881
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Fluxing of mantle carbon as a physical agent for metallogenic fertilization of the crust

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