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Presence of interplate channel layer controls of slip during and after the 2011 Tohoku-Oki earthquake through the frictional characteristics

There are significant differences between the middle and southern segments of the Japan Trench in terms of the seismic and aseismic slips on the plate interface and seismic velocity structures. Although the large coseismic slip of the 2011 Tohoku-Oki earthquake was limited to the middle segment, the...

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Bibliografiset tiedot
Julkaisussa:Sci Rep
Päätekijät: Nakata, Ryoko, Hori, Takane, Miura, Seiichi, Hino, Ryota
Aineistotyyppi: Artigo
Kieli:Inglês
Julkaistu: Nature Publishing Group UK 2021
Aiheet:
Linkit:https://ncbi.nlm.nih.gov/pmc/articles/PMC7979718/
https://ncbi.nlm.nih.gov/pubmed/33742049
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-021-86020-9
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