Liquiñe-Ofqui’s fast slipping intra-volcanic arc crustal faulting above the subducted Chile Ridge

The southernmost portion of the Liquiñe-Ofqui fault zone (LOFZ) lies within the proposed slab window which formed due to oblique subduction of the Chile Ridge in Patagonia. Mapping of paleo-surface ruptures, offsets, and lithological separations along the master fault allowed us to constrain geologi...

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Detalles Bibliográficos
Autores principales: De Pascale, Gregory P., Froude, Melanie, Penna, Ivanna, Hermanns, Reginald L., Sepúlveda, Sergio A., Moncada, Daniel, Persico, Mario, Easton, Gabriel, Villalobos, Angelo, Gutiérrez, Francisco
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8007613/
https://www.ncbi.nlm.nih.gov/pubmed/33782456
http://dx.doi.org/10.1038/s41598-021-86413-w

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8007613/
https://www.ncbi.nlm.nih.gov/pubmed/33782456
http://dx.doi.org/10.1038/s41598-021-86413-w

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