Deformation temperatures, vorticity of flow, and strain in the Moine thrust zone and Moine nappe: Reassessing the tectonic evolution of the Scandian foreland-hinterland transition zone

Journal of Structural Geology

Volumn 32, Issue 7, 2010, Pages 920-940

  Thigpen, J Ryan ^a   Law, Richard D ^a   Lloyd, Geoffrey E ^b   Brown, Summer J ^a  

^a VIRGINIA POLYTECHNIC INSTITUTE AND STATE UNIVERSITY   (United States)

^b UNIVERSITY OF LEEDS   (United Kingdom)

Author keywords

Assynt; Deformation temperatures; Moine; Scotland; Strain; Vorticity

Indexed keywords

ASSYNT; CONSTANT FLOW; CRUSTAL PROCESS; DEFORMATION TEMPERATURES; FLOW VORTICITY; MOINE; MYLONITES; OPENING ANGLE; OROGENIC WEDGE; PLANE STRAINS; PURE SHEAR; QUARTZ MICROSTRUCTURE; SCOTLAND; STRAIN DATA; TECTONIC EVOLUTION; THERMAL CHARACTERIZATION; THRUST ZONE; TRANSITION ZONES; VOLUME LOSS;

EXTRUSION; FABRICS; KINEMATICS; PARALLEL FLOW; QUARTZ; THREE DIMENSIONAL; VORTICITY;

DEFORMATION;

DEFORMATION; FORELAND BASIN; MICROSTRUCTURE; MYLONITE; NAPPE; OROGENY; QUARTZ; STRAIN; TECTONIC EVOLUTION; TECTONIC WEDGE; TEMPERATURE EFFECT; THRUST; TRANSITION ZONE; VORTICITY;

SCOTLAND; UNITED KINGDOM;

EID: 77957018892     PISSN: 01918141     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jsg.2010.05.001     Document Type: Article

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