A metasomatized lithospheric mantle control on the metallogenic signature of post-subduction magmatism

Hydrous and alkali rich magmas rise through the lithosphere and may host gold-rich ore deposits – a poorly understood process. Here, the authors present new chalcophile element data across a metallogenic section of the lithosphere and suggest a continuous or staged ascent of magmatic-hydrothermal se...

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Autores principales:	David A. Holwell, Marco Fiorentini, Iain McDonald, Yongjun Lu, Andrea Giuliani, Daniel J. Smith, Manuel Keith, Marek Locmelis
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2019
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/13dfbee8052a46c8893f54c59cc727f2
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spelling	oai:doaj.org-article:13dfbee8052a46c8893f54c59cc727f22021-12-02T14:39:58ZA metasomatized lithospheric mantle control on the metallogenic signature of post-subduction magmatism10.1038/s41467-019-11065-42041-1723https://doaj.org/article/13dfbee8052a46c8893f54c59cc727f22019-08-01T00:00:00Zhttps://doi.org/10.1038/s41467-019-11065-4https://doaj.org/toc/2041-1723Hydrous and alkali rich magmas rise through the lithosphere and may host gold-rich ore deposits – a poorly understood process. Here, the authors present new chalcophile element data across a metallogenic section of the lithosphere and suggest a continuous or staged ascent of magmatic-hydrothermal settings from mantle to upper crust.David A. HolwellMarco FiorentiniIain McDonaldYongjun LuAndrea GiulianiDaniel J. SmithManuel KeithMarek LocmelisNature PortfolioarticleScienceQENNature Communications, Vol 10, Iss 1, Pp 1-10 (2019)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q David A. Holwell Marco Fiorentini Iain McDonald Yongjun Lu Andrea Giuliani Daniel J. Smith Manuel Keith Marek Locmelis A metasomatized lithospheric mantle control on the metallogenic signature of post-subduction magmatism
description	Hydrous and alkali rich magmas rise through the lithosphere and may host gold-rich ore deposits – a poorly understood process. Here, the authors present new chalcophile element data across a metallogenic section of the lithosphere and suggest a continuous or staged ascent of magmatic-hydrothermal settings from mantle to upper crust.
format	article
author	David A. Holwell Marco Fiorentini Iain McDonald Yongjun Lu Andrea Giuliani Daniel J. Smith Manuel Keith Marek Locmelis
author_facet	David A. Holwell Marco Fiorentini Iain McDonald Yongjun Lu Andrea Giuliani Daniel J. Smith Manuel Keith Marek Locmelis
author_sort	David A. Holwell
title	A metasomatized lithospheric mantle control on the metallogenic signature of post-subduction magmatism
title_short	A metasomatized lithospheric mantle control on the metallogenic signature of post-subduction magmatism
title_full	A metasomatized lithospheric mantle control on the metallogenic signature of post-subduction magmatism
title_fullStr	A metasomatized lithospheric mantle control on the metallogenic signature of post-subduction magmatism
title_full_unstemmed	A metasomatized lithospheric mantle control on the metallogenic signature of post-subduction magmatism
title_sort	metasomatized lithospheric mantle control on the metallogenic signature of post-subduction magmatism
publisher	Nature Portfolio
publishDate	2019
url	https://doaj.org/article/13dfbee8052a46c8893f54c59cc727f2
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A metasomatized lithospheric mantle control on the metallogenic signature of post-subduction magmatism

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