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Lithospheric folding by flexural slip in subduction zones as source for reverse fault intraslab earthquakes
Subduction requires the permanent generation of a bend fold in the subducting slab which mechanics is not well understood. Lithospheric bending of subducting slabs was traditionally considered to be accommodated by orthogonal flexure, generating extensional outer rise earthquakes responsible of the...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group UK
2018
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5778079/ https://www.ncbi.nlm.nih.gov/pubmed/29358760 http://dx.doi.org/10.1038/s41598-018-19682-7 |