Preferred orientation of phyllosilicates: Comparison of fault gouge, shale and schist

Journal of Structural Geology

Volumn 32, Issue 4, 2010, Pages 478-489

  Wenk, Hans Rudolf ^a   Kanitpanyacharoen, Waruntorn ^a   Voltolini, Marco ^a  

^a UNIVERSITY OF CALIFORNIA   (United States)

Author keywords

Fault gouge; Phyllosilicate fabrics; Schist; Shale

Indexed keywords

AUTHIGENIC; CO-EXISTING; DIFFERENT MECHANISMS; DIFFRACTION IMAGES; DRILL HOLE; FAULT GOUGE; HETEROGENEOUS DEFORMATION; HIGH ENERGY SYNCHROTRON; LARGE TEXTURES; MICRO FABRIC; NORTH SEA; ORIENTATION DISTRIBUTIONS; OVERLAPPING PEAKS; PHYLLOSILICATE; PHYLLOSILICATE FABRICS; PRECIPITATION REACTION; PREFERRED ORIENTATIONS; RANDOM DISTRIBUTION; RECRYSTALLIZATIONS; SAN ANDREAS FAULT; SCHIST; SEDIMENTARY BASIN; STRESS FIELD;

DEFORMATION; DISSOLUTION; HOLOGRAPHIC INTERFEROMETRY; KAOLINITE; METAMORPHIC ROCKS; MICA; OXIDE MINERALS; QUARTZ; RIETVELD METHOD; SHALE; SILICATE MINERALS; TEXTURES;

FABRICS;

AUTHIGENIC MINERAL; CHEMICAL COMPOSITION; CLAY MINERAL; DECONVOLUTION; FAULT GOUGE; METAMORPHIC ROCK; PHYLLOSILICATE; PREFERRED ORIENTATION; RECRYSTALLIZATION; RIETVELD ANALYSIS; SCHIST; SEDIMENTARY BASIN; SHALE; STRESS FIELD;

ATLANTIC OCEAN; NORTH SEA;

EID: 77953139643     PISSN: 01918141     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jsg.2010.02.003     Document Type: Article

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