Fibrous clay mineral authigenesis induced by fluid-rock interaction in the Galera fault zone (Betic Cordillera, SE Spain) and its influence on fault gouge frictional properties
Fibrous clay mineral authigenesis induced by fluid-rock interaction in the Galera fault zone (Betic Cordillera, SE Spain) and its influence on fault gouge frictional properties
Authors
Keywords
Fault mechanics, Clay mineral authigenesis, Earthquake nucleation, SEM, Sepiolite, X-ray diffraction
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