Mode I microfracturing and fluid flow in damage zones: The key to distinguishing faults from slides

Journal of Structural Geology

Volumn 48, Issue , 2013, Pages 113-125

  Anders, Mark H ^a   Schneider, John R ^a,b   Scholz, Christopher H ^a   Losh, Steven ^c  

^a Department of Earth and Environmental Sciences   (United States)

^b UNIVERSITY OF WISCONSIN MADISON   (United States)

^c MINNESOTA STATE UNIVERSITY   (United States)

Author keywords

Cathodoluminescence; Detachment; Microfractures; Process zone; Slide blocks

Indexed keywords

ALLOCHTHONS; BASIN AND RANGE; CATASTROPHIC EMPLACEMENT; CRUSTAL EXTENSION; DAMAGE ZONES; DETACHMENT; DETACHMENT FAULT; DETACHMENT SURFACES; MICRO-FRACTURE; MICROFRACTURES; MICROFRACTURING; MULTIPLE FLUIDS; PROCESS ZONE; SLIDE BLOCKS; TECTONIC FAULTS; WYOMING;

CATHODOLUMINESCENCE; ROCKS;

FAULTING;

BRECCIA; CATHODOLUMINESCENCE; DETACHMENT FAULT; EMPLACEMENT; FAULT ZONE; FAULTING; FLUID FLOW; FRACTURE; INFILTRATION;

HEART MOUNTAIN; UNITED STATES; WYOMING;

EID: 84873718218     PISSN: 01918141     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jsg.2012.11.010     Document Type: Article

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