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Upper-plate conduits linked to plate boundary that hosts slow earthquakes - Nature Communications

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Upper-plate conduits linked to plate boundary that hosts slow earthquakes - Nature Communications

In shallow subduction zones, fluid behavior impacts various geodynamic processes capable of regulating slip behaviors and forming mud volcanoes. However, evidence of structures that control the fluid transfer within an overriding plate is limited and the physical properties at the source faults of slow earthquakes are poorly understood. Here we present high-resolution seismic velocity models and reflection images of the Hyuga-nada area, Japan, where the Kyushu-Palau ridge subducts.

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Upper-plate conduits linked to plate boundary that hosts slow earthquakes - Nature Communications

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Upper-plate conduits linked to plate boundary that hosts slow earthquakes - Nature Communications

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