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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2019
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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) |
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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 |
work_keys_str_mv |
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