High-temperature microstructures and rheology of deformed granite, Erzgebirge, Bohemian Massif

Journal of Structural Geology

Volumn 18, Issue 6, 1996, Pages 719-733

  Schulmann, Karel ^a   Mlčoch, Bedřich ^b   Melka, Radek ^a  

^a CHARLES UNIVERSITY   (Czech Republic)

^b CZECH GEOLOGICAL SURVEY   (Czech Republic)

Author keywords

[No Author keywords available]

Indexed keywords

AMPHIBOLITE FACIES; DEFORMATION; GRANITE; MICROSTRUCTURE; RHEOLOGY; STRAIN;

EUROPE, BOHEMIAN MASSIF, ERZGEBIRGE;

CRYSTAL MICROSTRUCTURE; CRYSTALLIZATION; FELDSPAR; GRAIN BOUNDARIES; GRAIN SIZE AND SHAPE; HIGH TEMPERATURE PROPERTIES; QUARTZ; RHEOLOGY; SHEAR DEFORMATION; STRAIN RATE;

AMPHIBOLITE FACIES CONDITIONS; INTERCONNECTED WEAK LAYER STRUCTURE; PORPHYRITIC GRANITOIDS; WEAKLY DEFORMED GRANITE;

GRANITE;

EID: 0029666724     PISSN: 01918141     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0191-8141(96)80007-1     Document Type: Article

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