Boninite-like intraplate magmas from Manihiki Plateau require ultra-depleted and enriched source components

Large igneous provinces may form very quickly, but compositions often differ. Here, the authors find that boninite-like rocks at Manihiki are a result of re-melting of an ultra-depleted source therefore putting into question that all boninitic rocks on Earth must be related to subduction processes.

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Autores principales:	Roman Golowin, Maxim Portnyagin, Kaj Hoernle, Folkmar Hauff, Andrey Gurenko, Dieter Garbe-Schönberg, Reinhard Werner, Simon Turner
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2017
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/a965bad3aafa470cb5fa9ecb0476aa98
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spelling	oai:doaj.org-article:a965bad3aafa470cb5fa9ecb0476aa982021-12-02T14:42:42ZBoninite-like intraplate magmas from Manihiki Plateau require ultra-depleted and enriched source components10.1038/ncomms143222041-1723https://doaj.org/article/a965bad3aafa470cb5fa9ecb0476aa982017-02-01T00:00:00Zhttps://doi.org/10.1038/ncomms14322https://doaj.org/toc/2041-1723Large igneous provinces may form very quickly, but compositions often differ. Here, the authors find that boninite-like rocks at Manihiki are a result of re-melting of an ultra-depleted source therefore putting into question that all boninitic rocks on Earth must be related to subduction processes.Roman GolowinMaxim PortnyaginKaj HoernleFolkmar HauffAndrey GurenkoDieter Garbe-SchönbergReinhard WernerSimon TurnerNature PortfolioarticleScienceQENNature Communications, Vol 8, Iss 1, Pp 1-10 (2017)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Roman Golowin Maxim Portnyagin Kaj Hoernle Folkmar Hauff Andrey Gurenko Dieter Garbe-Schönberg Reinhard Werner Simon Turner Boninite-like intraplate magmas from Manihiki Plateau require ultra-depleted and enriched source components
description	Large igneous provinces may form very quickly, but compositions often differ. Here, the authors find that boninite-like rocks at Manihiki are a result of re-melting of an ultra-depleted source therefore putting into question that all boninitic rocks on Earth must be related to subduction processes.
format	article
author	Roman Golowin Maxim Portnyagin Kaj Hoernle Folkmar Hauff Andrey Gurenko Dieter Garbe-Schönberg Reinhard Werner Simon Turner
author_facet	Roman Golowin Maxim Portnyagin Kaj Hoernle Folkmar Hauff Andrey Gurenko Dieter Garbe-Schönberg Reinhard Werner Simon Turner
author_sort	Roman Golowin
title	Boninite-like intraplate magmas from Manihiki Plateau require ultra-depleted and enriched source components
title_short	Boninite-like intraplate magmas from Manihiki Plateau require ultra-depleted and enriched source components
title_full	Boninite-like intraplate magmas from Manihiki Plateau require ultra-depleted and enriched source components
title_fullStr	Boninite-like intraplate magmas from Manihiki Plateau require ultra-depleted and enriched source components
title_full_unstemmed	Boninite-like intraplate magmas from Manihiki Plateau require ultra-depleted and enriched source components
title_sort	boninite-like intraplate magmas from manihiki plateau require ultra-depleted and enriched source components
publisher	Nature Portfolio
publishDate	2017
url	https://doaj.org/article/a965bad3aafa470cb5fa9ecb0476aa98
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Boninite-like intraplate magmas from Manihiki Plateau require ultra-depleted and enriched source components

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