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Deep slab seismicity limited by rate of deformation in the transition zone

Deep earthquakes within subducting tectonic plates (slabs) are enigmatic because they appear similar to shallow earthquakes but must occur by a different mechanism. Previous attempts to explain the depth distribution of deep earthquakes in terms of the temperature at which possible triggering mechan...

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Detalles Bibliográficos
Autor principal: Billen, Magali I.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2020
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7385466/
https://www.ncbi.nlm.nih.gov/pubmed/32766442
http://dx.doi.org/10.1126/sciadv.aaz7692

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