טוען...
Cascadia low frequency earthquakes at the base of an overpressured subduction shear zone
In subduction zones, landward dipping regions of low shear wave velocity and elevated Poisson’s ratio, which can extend to at least 120 km depth, are interpreted to be all or part of the subducting igneous oceanic crust. This crust is considered to be overpressured, because fluids within it are trap...
שמור ב:
| הוצא לאור ב: | Nat Commun |
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| Main Authors: | , , , |
| פורמט: | Artigo |
| שפה: | Inglês |
| יצא לאור: |
Nature Publishing Group UK
2020
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| נושאים: | |
| גישה מקוונת: | https://ncbi.nlm.nih.gov/pmc/articles/PMC7398906/ https://ncbi.nlm.nih.gov/pubmed/32747641 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-020-17609-3 |
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