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Lasting mantle scars lead to perennial plate tectonics
Mid-ocean ridges, transform faults, subduction and continental collisions form the conventional theory of plate tectonics to explain non-rigid behaviour at plate boundaries. However, the theory does not explain directly the processes involved in intraplate deformation and seismicity. Recently, damag...
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| Publicat a: | Nat Commun |
|---|---|
| Autors principals: | , , |
| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Nature Publishing Group
2016
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4906409/ https://ncbi.nlm.nih.gov/pubmed/27282541 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms11834 |
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