Multiscale anisotropy controlled by folding: the example of the Chaudrons fold (Corbières, France)

Journal of Structural Geology

Volumn 28, Issue 4, 2006, Pages 549-560

  Louis, Laurent ^a,b   Robion, Philippe ^a   David, Christian ^a   Frizon de Lamotte, Dominique ^a  

^a UNIVERSITÉ DE CERGY PONTOISE   (France)

^b STONY BROOK UNIVERSITY   (United States)

Author keywords

Anisotropy; Cleavage; Magnetic susceptibility; P wave velocity; Pressure solution

Indexed keywords

ANISOTROPY; CALCITE; MAGNETIC SUSCEPTIBILITY; MICROSTRUCTURE; PRESSURE; SEISMIC WAVES;

CLEAVAGE; MULTISCALE ANISOTROPY; P-WAVE VELOCITY; PRESSURE SOLUTION; SILICOCLASTIC CONTINENTAL DEPOSITS;

STRUCTURAL GEOLOGY;

ANTICLINE; CLEAVAGE; DEFORMATION; FOLD; FOLDING; MAGNETIC ANISOTROPY; MAGNETIC SUSCEPTIBILITY; P-WAVE; PRESSURE SOLUTION; WAVE VELOCITY;

EURASIA; EUROPE; FRANCE; WESTERN EUROPE;

EID: 84984554863     PISSN: 01918141     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jsg.2006.01.002     Document Type: Article

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