Melting of the continental crust during orogenesis: The thermal, rheological, and compositional consequences of melt transport from lower to upper continental crust

Canadian Journal of Earth Sciences

Volumn 47, Issue 5, 2010, Pages 655-694

  Brown, Michael ^a  

^a University of Maryland   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

ANATEXIS; AQUEOUS FLUIDS; BRITTLE-DUCTILE TRANSITION ZONE; CONTINENTAL CRUSTS; EXSOLUTION; FRACTURE NETWORK; HIGH STRAIN DEFORMATION; HIGHER TEMPERATURES; LATERAL EXPANSION; MECHANICAL INSTABILITIES; MELT COMPOSITIONS; MELT EXTRACTION; MELT FLOW; MELT LOSS; MELT MIGRATION; MELT PRODUCTION; MELT VOLUME; MESOSCALE; OROGENIC BELTS; PERITECTIC; PERMEABILITY CONTROL; PLUTONS; PRESSURE-TEMPERATURE-TIME PATHS; SHEAR FAILURE; STRONG ANISOTROPY; UPPER CONTINENTAL CRUST;

ANISOTROPY; CRYSTALLIZATION; DEFORMATION; DUCTILE FRACTURE; FLUIDS; GRAIN BOUNDARIES; HYDRATES; MELTING; PHASE EQUILIBRIA; RHEOLOGY; THERMAL EXPANSION;

BRITTLE FRACTURE;

ANATEXIS; CONTINENTAL CRUST; CONVERGENT MARGIN; CRYSTALLIZATION; DEFORMATION; MELTING; OROGENY; OUTCROP; PELITE; PLUTON; RHEOLOGY; THERMAL ALTERATION; TRANSITION ZONE;

EID: 77958142689     PISSN: 00084077     EISSN: 14803313     Source Type: Journal    
DOI: 10.1139/E09-057     Document Type: Article

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