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The paper discusses the role of fluid overpressures in the lower crustal seismogenic zone and their influence on large crustal earthquakes through fault-valve action. It presents geological and geophysical evidence supporting the existence of localized fluid overpressuring, particularly in compressional–transpressional tectonic regimes, which can lead to dual-driven fault failure. The study emphasizes the need for systematic evaluation of these associations across different tectonic settings to understand t

Author

riccaque

Language

EN