Lithological control on the deformation mechanism and the mode of fault slip on the Longitudinal Valley Fault, Taiwan

Tectonophysics

Volumn 632, Issue C, 2014, Pages 48-63

  Thomas, Marion Y ^a   Avouac, Jean Philippe ^a   Gratier, Jean Pierre ^b,c   Lee, Jian Cheng ^d  

^a CALIFORNIA INSTITUTE OF TECHNOLOGY   (United States)

^b UNIVERSITÉ GRENOBLE ALPES   (France)

^c CNRS   (France)

^d INSTITUTE OF EARTH SCIENCES   (Taiwan)

Author keywords

Aseismic slip; Deformation mechanism; Frictional sliding; Lichi M lange; Longitudinal valley fault; Pressure solution creep

Indexed keywords

CREEP; DEFORMATION; FRICTION; GRAIN BOUNDARIES; GRINDING (COMMINUTION); KAOLINITE; LANDFORMS; LITHOLOGY; MECHANICAL PROPERTIES; STRUCTURAL GEOLOGY;

ASEISMIC BEHAVIORS; ASEISMIC SLIP; CONTINENTAL SHELVES; DEFORMATION MECHANISM; FRICTIONAL SLIDING; INTERNAL DEFORMATION; MICROSTRUCTURAL INVESTIGATION; PRESSURE-SOLUTION CREEP;

FAULT SLIPS;

CONTINENTAL SHELF; CREEP; DEFORMATION MECHANISM; FAULT GOUGE; FAULT SLIP; FRICTION; LITHOLOGY; MELANGE; PHILIPPINE SEA PLATE;

LONGITUDINAL VALLEY; TAIWAN;

EID: 84919471832     PISSN: 00401951     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.tecto.2014.05.038     Document Type: Article

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