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...
Guardado en:
Autores principales: | , , , , , , |
---|---|
Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2020
|
Materias: | |
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 |