Frictional Melting in Hydrothermal Fluid‐Rich Faults: Field and Experimental Evidence From the Bolfín Fault Zone (Chile)

Tectonic pseudotachylytes are thought to be unique to certain water‐deficient seismogenic environments and their presence is considered to be rare in the geological record. Here, we present field and experimental evidence that frictional melting can occur in hydrothermal fluid‐rich faults hosted in...

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Detalles Bibliográficos
Autores principales: Gomila, R., Fondriest, M., Jensen, E., Spagnuolo, E., Masoch, S., Mitchell, T. M., Magnarini, G., Bistacchi, A., Mittempergher, S., Faulkner, D., Cembrano, J., Di Toro, G.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2021
Materias:
Research Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8365670/
https://www.ncbi.nlm.nih.gov/pubmed/34434077
http://dx.doi.org/10.1029/2021GC009743

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8365670/
https://www.ncbi.nlm.nih.gov/pubmed/34434077
http://dx.doi.org/10.1029/2021GC009743

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