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Frictional melting mechanisms of rocks during earthquake fault slip

Rapid slip, at rates in the order of 1 m/s or more, may induce frictional melting in rocks during earthquakes. The short-lived melting has been thought to be a disequilibrium process, for decades. We conducted frictional melting experiments on acidic, basic, and ultrabasic silicate rocks at a slip r...

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Detalles Bibliográficos
Autores principales: Woo, Sangwoo, Han, Raehee, Oohashi, Kiyokazu
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2023
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10397195/
https://www.ncbi.nlm.nih.gov/pubmed/37532914
http://dx.doi.org/10.1038/s41598-023-39752-9