Continuous plate subduction marked by the rise of alkali magmatism 2.1 billion years ago

The point in time in which the ancient stagnant-lid tectonic regime with episodic plate subduction changed to continuous plate subduction is still topic of scientific debate. Here, the authors present vast geochemical dataset covering the last 3.5 billion years of Earth’s history and date the onset...

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Autores principales:	He Liu, Wei-dong Sun, Robert Zartman, Ming Tang
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2019
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/ba309415c5ec4e6faebfaa1179e70ed7
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spelling	oai:doaj.org-article:ba309415c5ec4e6faebfaa1179e70ed72021-12-02T15:36:22ZContinuous plate subduction marked by the rise of alkali magmatism 2.1 billion years ago10.1038/s41467-019-11329-z2041-1723https://doaj.org/article/ba309415c5ec4e6faebfaa1179e70ed72019-07-01T00:00:00Zhttps://doi.org/10.1038/s41467-019-11329-zhttps://doaj.org/toc/2041-1723The point in time in which the ancient stagnant-lid tectonic regime with episodic plate subduction changed to continuous plate subduction is still topic of scientific debate. Here, the authors present vast geochemical dataset covering the last 3.5 billion years of Earth’s history and date the onset of continuous subduction to about 2.1 billion years ago.He LiuWei-dong SunRobert ZartmanMing TangNature PortfolioarticleScienceQENNature Communications, Vol 10, Iss 1, Pp 1-8 (2019)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q He Liu Wei-dong Sun Robert Zartman Ming Tang Continuous plate subduction marked by the rise of alkali magmatism 2.1 billion years ago
description	The point in time in which the ancient stagnant-lid tectonic regime with episodic plate subduction changed to continuous plate subduction is still topic of scientific debate. Here, the authors present vast geochemical dataset covering the last 3.5 billion years of Earth’s history and date the onset of continuous subduction to about 2.1 billion years ago.
format	article
author	He Liu Wei-dong Sun Robert Zartman Ming Tang
author_facet	He Liu Wei-dong Sun Robert Zartman Ming Tang
author_sort	He Liu
title	Continuous plate subduction marked by the rise of alkali magmatism 2.1 billion years ago
title_short	Continuous plate subduction marked by the rise of alkali magmatism 2.1 billion years ago
title_full	Continuous plate subduction marked by the rise of alkali magmatism 2.1 billion years ago
title_fullStr	Continuous plate subduction marked by the rise of alkali magmatism 2.1 billion years ago
title_full_unstemmed	Continuous plate subduction marked by the rise of alkali magmatism 2.1 billion years ago
title_sort	continuous plate subduction marked by the rise of alkali magmatism 2.1 billion years ago
publisher	Nature Portfolio
publishDate	2019
url	https://doaj.org/article/ba309415c5ec4e6faebfaa1179e70ed7
work_keys_str_mv	AT heliu continuousplatesubductionmarkedbytheriseofalkalimagmatism21billionyearsago AT weidongsun continuousplatesubductionmarkedbytheriseofalkalimagmatism21billionyearsago AT robertzartman continuousplatesubductionmarkedbytheriseofalkalimagmatism21billionyearsago AT mingtang continuousplatesubductionmarkedbytheriseofalkalimagmatism21billionyearsago
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Continuous plate subduction marked by the rise of alkali magmatism 2.1 billion years ago

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