Complex fault interaction controls continental rifting

Rifted margins mark a transition from continents to oceans and contain in their architecture a record of their rift history. Recent investigations of rift architecture have suggested that multiphase deformation of the crust and mantle lithosphere leads to the formation of distinct margin domains. Th...

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Detalles Bibliográficos
Autores principales: Naliboff, John B., Buiter, Susanne J. H., Péron-Pinvidic, Gwenn, Osmundsen, Per Terje, Tetreault, Joya
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2017
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5661748/
https://www.ncbi.nlm.nih.gov/pubmed/29081494
http://dx.doi.org/10.1038/s41467-017-00904-x

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5661748/
https://www.ncbi.nlm.nih.gov/pubmed/29081494
http://dx.doi.org/10.1038/s41467-017-00904-x

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