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Mapping the evolving strain field during continental breakup from crustal anisotropy in the Afar Depression

Rifting of the continents leading to plate rupture occurs by a combination of mechanical deformation and magma intrusion, yet the spatial and temporal scales over which these alternate mechanisms localize extensional strain remain controversial. Here we quantify anisotropy of the upper crust across...

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Detalhes bibliográficos
Main Authors: Keir, Derek, Belachew, M., Ebinger, C.J., Kendall, J.-M., Hammond, J.O.S., Stuart, G.W., Ayele, A., Rowland, J.V.
Formato: Artigo
Idioma:Inglês
Publicado em: Nature Publishing Group 2011
Assuntos:
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC3104516/
https://ncbi.nlm.nih.gov/pubmed/21505441
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms1287
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