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What is Chile Subduction Zone Fluid Pressure Impact about?

This study examines the relationship between pore fluid pressure and locking patterns along the subduction zone interface that ruptured during the 2010 Maule, Chile earthquake. High resolution seismic tomography revealed variations in seismic P- and S-wave velocity ratios (Vp/Vs) along the interface, which are interpreted as variations in pore fluid pressure. Areas with high Vp/Vs, and thus high pore pressure, correlated spatially with poorly locked areas that slipped aseismically. In contrast, areas with l

Author

hüseyin burak göktaş

Language

EN