Seismogenesis of dual subduction beneath Kanto, central Japan controlled by fluid release


Dual subduction represents an unusual case of subduction where one oceanic plate subducts on top of another, creating a highly complex tectonic setting. Because of the complex interaction between the two subducted plates, the origin of seismicity in such region is still not fully understood. Here we investigate the thermal structure of dual subduction… (More)
DOI: 10.1038/s41598-017-16818-z

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