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The stress-loading of faults to failure in earthquakes is driven by regional tectonics, but is also influenced by fault interaction during earthquakes,
PALEO-“STRESS” ANALYSIS FROM FAULT DATA Slicken-lines on a fault plane represent the direction of some relative displacement between the two
compilations, it was assumed, that patterns of stress orientation on a regional scale are more or less consistent within tectonic plates (Coblentz and