Fluid-assisted grain size reduction leads to strain localization in oceanic transform faults

Oceanic Transform Faults are major plate boundaries representing the most seismogenic part of the mid ocean ridge system. Nonetheless, their structure and deformation mechanisms at depth are largely unknown due to rare exposures of deep sections. Here we study the mineral fabric of deformed mantle p...

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Detalles Bibliográficos
Autores principales: Bickert, Manon, Kaczmarek, Mary-Alix, Brunelli, Daniele, Maia, Marcia, Campos, Thomas F. C., Sichel, Susanna E.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2023
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10333221/
https://www.ncbi.nlm.nih.gov/pubmed/37429902
http://dx.doi.org/10.1038/s41467-023-39556-5

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10333221/
https://www.ncbi.nlm.nih.gov/pubmed/37429902
http://dx.doi.org/10.1038/s41467-023-39556-5

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