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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...

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Gorde:
Xehetasun bibliografikoak
Argitaratua izan da:Nat Commun
Egile Nagusiak: Calvert, Andrew J., Bostock, Michael G., Savard, Geneviève, Unsworth, Martyn J.
Formatua: Artigo
Hizkuntza:Inglês
Argitaratua: Nature Publishing Group UK 2020
Gaiak:
Sarrera elektronikoa: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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