Limited and localized magmatism in the Central Atlantic Magmatic Province

The Central Atlantic Magmatic Province is the most aerially extensive magmatic event in Earth’s history, yet few constraints exist on the volumes of intrusions at depth. Here, the authors find limited intrusive volumes beneath the South Georgia Rift, consistent with modest potential mantle temperatu...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: R. E. Marzen, D. J. Shillington, D. Lizarralde, J. H. Knapp, D. M. Heffner, J. K. Davis, S. H. Harder
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2020
Materias:
Q
Acceso en línea:https://doaj.org/article/0187946bb48c46d591dadf58879a1a26
Etiquetas: Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
id oai:doaj.org-article:0187946bb48c46d591dadf58879a1a26
record_format dspace
spelling oai:doaj.org-article:0187946bb48c46d591dadf58879a1a262021-12-02T16:15:09ZLimited and localized magmatism in the Central Atlantic Magmatic Province10.1038/s41467-020-17193-62041-1723https://doaj.org/article/0187946bb48c46d591dadf58879a1a262020-07-01T00:00:00Zhttps://doi.org/10.1038/s41467-020-17193-6https://doaj.org/toc/2041-1723The Central Atlantic Magmatic Province is the most aerially extensive magmatic event in Earth’s history, yet few constraints exist on the volumes of intrusions at depth. Here, the authors find limited intrusive volumes beneath the South Georgia Rift, consistent with modest potential mantle temperatures (<1500 °C) related to syn-rift decompression melting.R. E. MarzenD. J. ShillingtonD. LizarraldeJ. H. KnappD. M. HeffnerJ. K. DavisS. H. HarderNature PortfolioarticleScienceQENNature Communications, Vol 11, Iss 1, Pp 1-8 (2020)
institution DOAJ
collection DOAJ
language EN
topic Science
Q
spellingShingle Science
Q
R. E. Marzen
D. J. Shillington
D. Lizarralde
J. H. Knapp
D. M. Heffner
J. K. Davis
S. H. Harder
Limited and localized magmatism in the Central Atlantic Magmatic Province
description The Central Atlantic Magmatic Province is the most aerially extensive magmatic event in Earth’s history, yet few constraints exist on the volumes of intrusions at depth. Here, the authors find limited intrusive volumes beneath the South Georgia Rift, consistent with modest potential mantle temperatures (<1500 °C) related to syn-rift decompression melting.
format article
author R. E. Marzen
D. J. Shillington
D. Lizarralde
J. H. Knapp
D. M. Heffner
J. K. Davis
S. H. Harder
author_facet R. E. Marzen
D. J. Shillington
D. Lizarralde
J. H. Knapp
D. M. Heffner
J. K. Davis
S. H. Harder
author_sort R. E. Marzen
title Limited and localized magmatism in the Central Atlantic Magmatic Province
title_short Limited and localized magmatism in the Central Atlantic Magmatic Province
title_full Limited and localized magmatism in the Central Atlantic Magmatic Province
title_fullStr Limited and localized magmatism in the Central Atlantic Magmatic Province
title_full_unstemmed Limited and localized magmatism in the Central Atlantic Magmatic Province
title_sort limited and localized magmatism in the central atlantic magmatic province
publisher Nature Portfolio
publishDate 2020
url https://doaj.org/article/0187946bb48c46d591dadf58879a1a26
work_keys_str_mv AT remarzen limitedandlocalizedmagmatisminthecentralatlanticmagmaticprovince
AT djshillington limitedandlocalizedmagmatisminthecentralatlanticmagmaticprovince
AT dlizarralde limitedandlocalizedmagmatisminthecentralatlanticmagmaticprovince
AT jhknapp limitedandlocalizedmagmatisminthecentralatlanticmagmaticprovince
AT dmheffner limitedandlocalizedmagmatisminthecentralatlanticmagmaticprovince
AT jkdavis limitedandlocalizedmagmatisminthecentralatlanticmagmaticprovince
AT shharder limitedandlocalizedmagmatisminthecentralatlanticmagmaticprovince
_version_ 1718384270922219520