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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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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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American Association for the Advancement of Science
2020
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| 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 |