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- W2655200024 abstract "Both fracture permeability and fluid flow velocity can alter as a result of sudden strain changes associated with earthquake fault rupture. Testing the hydrological signatures of numerous earthquakes worldwide against simple strain models has provided the foundation of a methodology for comprehending this important hazard for hardrock repositories. The spatial extent and character of the strainfield is dependent on the tectonic style of faulting: major normal fault earthquakes have the most marked hydrological impact. Near-field hydrological changes, originating at the fault, can reflect strain changes in excess of 10 -3 producing an almost explosive release of water. At far field distances of up to 60km residual strains can be sustained in excess of 10 -5 while at greater distances strain is concentrated on a few susceptible and isolated fractures." @default.
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- W2655200024 date "1991-01-01" @default.
- W2655200024 modified "2023-09-24" @default.
- W2655200024 title "An Empirical Data Base for the Investigation of Earthquake-Related Changes in Crustal Hydrology" @default.
- W2655200024 hasPublicationYear "1991" @default.
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