Crystal and melt inclusion timescales reveal the evolution of magma migration before eruption

Volatile contents in melt inclusions can be used to unravel magma migration and degassing. Here, the authors use olivine chronometry and melt inclusion data from the 2008 Llaima eruption and find that magma intrusion occurred 4 years before the eruption and reached a depth of 3–4 km, 6 months before...

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Autores principales:	Dawn C. S. Ruth, Fidel Costa, Caroline Bouvet de Maisonneuve, Luis Franco, Joaquin A. Cortés, Eliza S. Calder
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2018
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/a6056114edac4323a124cc708376bea4
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spelling	oai:doaj.org-article:a6056114edac4323a124cc708376bea42021-12-02T17:32:44ZCrystal and melt inclusion timescales reveal the evolution of magma migration before eruption10.1038/s41467-018-05086-82041-1723https://doaj.org/article/a6056114edac4323a124cc708376bea42018-07-01T00:00:00Zhttps://doi.org/10.1038/s41467-018-05086-8https://doaj.org/toc/2041-1723Volatile contents in melt inclusions can be used to unravel magma migration and degassing. Here, the authors use olivine chronometry and melt inclusion data from the 2008 Llaima eruption and find that magma intrusion occurred 4 years before the eruption and reached a depth of 3–4 km, 6 months before the eruption.Dawn C. S. RuthFidel CostaCaroline Bouvet de MaisonneuveLuis FrancoJoaquin A. CortésEliza S. CalderNature PortfolioarticleScienceQENNature Communications, Vol 9, Iss 1, Pp 1-9 (2018)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Dawn C. S. Ruth Fidel Costa Caroline Bouvet de Maisonneuve Luis Franco Joaquin A. Cortés Eliza S. Calder Crystal and melt inclusion timescales reveal the evolution of magma migration before eruption
description	Volatile contents in melt inclusions can be used to unravel magma migration and degassing. Here, the authors use olivine chronometry and melt inclusion data from the 2008 Llaima eruption and find that magma intrusion occurred 4 years before the eruption and reached a depth of 3–4 km, 6 months before the eruption.
format	article
author	Dawn C. S. Ruth Fidel Costa Caroline Bouvet de Maisonneuve Luis Franco Joaquin A. Cortés Eliza S. Calder
author_facet	Dawn C. S. Ruth Fidel Costa Caroline Bouvet de Maisonneuve Luis Franco Joaquin A. Cortés Eliza S. Calder
author_sort	Dawn C. S. Ruth
title	Crystal and melt inclusion timescales reveal the evolution of magma migration before eruption
title_short	Crystal and melt inclusion timescales reveal the evolution of magma migration before eruption
title_full	Crystal and melt inclusion timescales reveal the evolution of magma migration before eruption
title_fullStr	Crystal and melt inclusion timescales reveal the evolution of magma migration before eruption
title_full_unstemmed	Crystal and melt inclusion timescales reveal the evolution of magma migration before eruption
title_sort	crystal and melt inclusion timescales reveal the evolution of magma migration before eruption
publisher	Nature Portfolio
publishDate	2018
url	https://doaj.org/article/a6056114edac4323a124cc708376bea4
work_keys_str_mv	AT dawncsruth crystalandmeltinclusiontimescalesrevealtheevolutionofmagmamigrationbeforeeruption AT fidelcosta crystalandmeltinclusiontimescalesrevealtheevolutionofmagmamigrationbeforeeruption AT carolinebouvetdemaisonneuve crystalandmeltinclusiontimescalesrevealtheevolutionofmagmamigrationbeforeeruption AT luisfranco crystalandmeltinclusiontimescalesrevealtheevolutionofmagmamigrationbeforeeruption AT joaquinacortes crystalandmeltinclusiontimescalesrevealtheevolutionofmagmamigrationbeforeeruption AT elizascalder crystalandmeltinclusiontimescalesrevealtheevolutionofmagmamigrationbeforeeruption
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Crystal and melt inclusion timescales reveal the evolution of magma migration before eruption

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