Stress-state evolution of the brittle upper crust during compressional tectonic inversion as defined by successive quartz vein types (High-Ardenne slate belt, Germany)

Journal of the Geological Society

Volumn 168, Issue 2, 2011, Pages 407-422

  van Noten, Koen ^a   Muchez, Philippe ^a   Sintubin, Manuel ^a  

^a UNIVERSITY OF LEUVEN   (Belgium)

Author keywords

[No Author keywords available]

Indexed keywords

COMPRESSIONAL; COMPRESSIONAL TECTONICS; DEVONIANS; DIFFERENTIAL STRESS; EXTENSIONAL STRESS; FLUID PRESSURES; FOLD-AND-THRUST BELTS; GERMANY; LOW-GRADE METAMORPHIC; OVER-PRESSURES; PRESSURE-TEMPERATURE CONDITIONS; QUARTZ VEIN; REGIONAL FOLDS; SEDIMENTARY BASIN; STATE EVOLUTIONS; STRESS REGIME; UPPER CRUST; VARISCAN;

FLUIDS; KINEMATICS; QUARTZ; SLATE;

TECTONICS;

FOLD AND THRUST BELT; HERCYNIAN OROGENY; INVERSION TECTONICS; KINEMATICS; QUARTZ VEIN; TECTONIC EVOLUTION; UPPER CRUST;

GERMANY;

EID: 79952274765     PISSN: 00167649     EISSN: None     Source Type: Journal    
DOI: 10.1144/0016-76492010-112     Document Type: Article

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