Semibrittle seismic deformation in high-temperature mantle mylonite shear zone along the Romanche transform fault

Oceanic transform faults, a key element of plate tectonics, represent the first-order discontinuities along mid-ocean ridges, host large earthquakes, and induce extreme thermal gradients in lithosphere. However, the thermal structure along transform faults and its effects on earthquake generation ar...

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Detalles Bibliográficos
Autores principales: Yu, Zhiteng, Singh, Satish C., Gregory, Emma P. M., Maia, Marcia, Wang, Zhikai, Brunelli, Daniele
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2021
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8034845/
https://www.ncbi.nlm.nih.gov/pubmed/33837085
http://dx.doi.org/10.1126/sciadv.abf3388

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8034845/
https://www.ncbi.nlm.nih.gov/pubmed/33837085
http://dx.doi.org/10.1126/sciadv.abf3388

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