Superplume mantle tracked isotopically the length of Africa from the Indian Ocean to the Red Sea

Low seismic velocity anomalies reveal a complex scenario of plume upwellings from a deep thermo-chemical anomaly (superplume) in the mantle below the East African Rift, however, geophysical observations alone are insufficient to identify the extent of plume influence on the magmatism along the rift....

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Autores principales: John M. O’Connor, Wilfried Jokat, Marcel Regelous, Klaudia F. Kuiper, Daniel P. Miggins, Anthony A. P. Koppers
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2019
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Acceso en línea:https://doaj.org/article/c88bb629158243038360d0023195afb1
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spelling oai:doaj.org-article:c88bb629158243038360d0023195afb12021-12-02T14:38:37ZSuperplume mantle tracked isotopically the length of Africa from the Indian Ocean to the Red Sea10.1038/s41467-019-13181-72041-1723https://doaj.org/article/c88bb629158243038360d0023195afb12019-12-01T00:00:00Zhttps://doi.org/10.1038/s41467-019-13181-7https://doaj.org/toc/2041-1723Low seismic velocity anomalies reveal a complex scenario of plume upwellings from a deep thermo-chemical anomaly (superplume) in the mantle below the East African Rift, however, geophysical observations alone are insufficient to identify the extent of plume influence on the magmatism along the rift. Here, the authors use Sr-Nd-Pb isotope data to show that superplume mantle underlies the entire rift system, from the Red Sea to the Indian Ocean south of Mozambique.John M. O’ConnorWilfried JokatMarcel RegelousKlaudia F. KuiperDaniel P. MigginsAnthony A. P. KoppersNature PortfolioarticleScienceQENNature Communications, Vol 10, Iss 1, Pp 1-13 (2019)
institution DOAJ
collection DOAJ
language EN
topic Science
Q
spellingShingle Science
Q
John M. O’Connor
Wilfried Jokat
Marcel Regelous
Klaudia F. Kuiper
Daniel P. Miggins
Anthony A. P. Koppers
Superplume mantle tracked isotopically the length of Africa from the Indian Ocean to the Red Sea
description Low seismic velocity anomalies reveal a complex scenario of plume upwellings from a deep thermo-chemical anomaly (superplume) in the mantle below the East African Rift, however, geophysical observations alone are insufficient to identify the extent of plume influence on the magmatism along the rift. Here, the authors use Sr-Nd-Pb isotope data to show that superplume mantle underlies the entire rift system, from the Red Sea to the Indian Ocean south of Mozambique.
format article
author John M. O’Connor
Wilfried Jokat
Marcel Regelous
Klaudia F. Kuiper
Daniel P. Miggins
Anthony A. P. Koppers
author_facet John M. O’Connor
Wilfried Jokat
Marcel Regelous
Klaudia F. Kuiper
Daniel P. Miggins
Anthony A. P. Koppers
author_sort John M. O’Connor
title Superplume mantle tracked isotopically the length of Africa from the Indian Ocean to the Red Sea
title_short Superplume mantle tracked isotopically the length of Africa from the Indian Ocean to the Red Sea
title_full Superplume mantle tracked isotopically the length of Africa from the Indian Ocean to the Red Sea
title_fullStr Superplume mantle tracked isotopically the length of Africa from the Indian Ocean to the Red Sea
title_full_unstemmed Superplume mantle tracked isotopically the length of Africa from the Indian Ocean to the Red Sea
title_sort superplume mantle tracked isotopically the length of africa from the indian ocean to the red sea
publisher Nature Portfolio
publishDate 2019
url https://doaj.org/article/c88bb629158243038360d0023195afb1
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