The causes of spatiotemporal variations in erupted fluxes and compositions along a volcanic arc

The primary causes of dramatic variations in volcanic flux and composition along strike in subduction zones remain largely unknown. Here we use a promising new approach to show that along-strike volcanic variability in the Quaternary Cascades Arc is primarily due to variations in the flux of basalt...

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Autores principales:	C. B. Till, A. J. R. Kent, G. A. Abers, H. A. Janiszewski, J. B. Gaherty, B. W. Pitcher
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2019
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/42bec1a09e1b4049aeca6cc653d33e68
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spelling	oai:doaj.org-article:42bec1a09e1b4049aeca6cc653d33e682021-12-02T14:39:42ZThe causes of spatiotemporal variations in erupted fluxes and compositions along a volcanic arc10.1038/s41467-019-09113-02041-1723https://doaj.org/article/42bec1a09e1b4049aeca6cc653d33e682019-03-01T00:00:00Zhttps://doi.org/10.1038/s41467-019-09113-0https://doaj.org/toc/2041-1723The primary causes of dramatic variations in volcanic flux and composition along strike in subduction zones remain largely unknown. Here we use a promising new approach to show that along-strike volcanic variability in the Quaternary Cascades Arc is primarily due to variations in the flux of basalt into the base of the crust, rather than crustal magma storage.C. B. TillA. J. R. KentG. A. AbersH. A. JaniszewskiJ. B. GahertyB. W. PitcherNature PortfolioarticleScienceQENNature Communications, Vol 10, Iss 1, Pp 1-12 (2019)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q C. B. Till A. J. R. Kent G. A. Abers H. A. Janiszewski J. B. Gaherty B. W. Pitcher The causes of spatiotemporal variations in erupted fluxes and compositions along a volcanic arc
description	The primary causes of dramatic variations in volcanic flux and composition along strike in subduction zones remain largely unknown. Here we use a promising new approach to show that along-strike volcanic variability in the Quaternary Cascades Arc is primarily due to variations in the flux of basalt into the base of the crust, rather than crustal magma storage.
format	article
author	C. B. Till A. J. R. Kent G. A. Abers H. A. Janiszewski J. B. Gaherty B. W. Pitcher
author_facet	C. B. Till A. J. R. Kent G. A. Abers H. A. Janiszewski J. B. Gaherty B. W. Pitcher
author_sort	C. B. Till
title	The causes of spatiotemporal variations in erupted fluxes and compositions along a volcanic arc
title_short	The causes of spatiotemporal variations in erupted fluxes and compositions along a volcanic arc
title_full	The causes of spatiotemporal variations in erupted fluxes and compositions along a volcanic arc
title_fullStr	The causes of spatiotemporal variations in erupted fluxes and compositions along a volcanic arc
title_full_unstemmed	The causes of spatiotemporal variations in erupted fluxes and compositions along a volcanic arc
title_sort	causes of spatiotemporal variations in erupted fluxes and compositions along a volcanic arc
publisher	Nature Portfolio
publishDate	2019
url	https://doaj.org/article/42bec1a09e1b4049aeca6cc653d33e68
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The causes of spatiotemporal variations in erupted fluxes and compositions along a volcanic arc

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