Aborted propagation of the Ethiopian rift caused by linkage with the Kenyan rift

Continuous continental rift zones evolve from enigmatic interactions between individual propagating rift segments. Here, the authors document progressive focusing of tectonic and magmatic activity caused by interactions between the Kenyan and Ethiopian rift segments of the East African Rift.

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Detalles Bibliográficos
Autores principales: Giacomo Corti, Raffaello Cioni, Zara Franceschini, Federico Sani, Stéphane Scaillet, Paola Molin, Ilaria Isola, Francesco Mazzarini, Sascha Brune, Derek Keir, Asfaw Erbello, Ameha Muluneh, Finnigan Illsley-Kemp, Anne Glerum
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2019
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Acceso en línea:https://doaj.org/article/ddfc729fd6204591beb6aa4e12a80aff
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Descripción
Sumario:Continuous continental rift zones evolve from enigmatic interactions between individual propagating rift segments. Here, the authors document progressive focusing of tectonic and magmatic activity caused by interactions between the Kenyan and Ethiopian rift segments of the East African Rift.