Implication of corona formation in a metatroctolite to the granulite facies overprint of HP-UHP rocks in the Moldanubian Zone (Bohemian Massif)

Journal of Metamorphic Geology

Volumn 33, Issue 3, 2015, Pages 295-310

  Faryad, S W ^a   Kachlik V ^a   Slama J ^b,c   Hoinkes, G ^d  

^a CHARLES UNIVERSITY   (Czech Republic)

^b UNIVERSITY OF BERGEN   (Norway)

^c INSTITUTE OF GEOLOGY   (Czech Republic)

^d UNIVERSITY OF GRAZ   (Austria)

Author keywords

Coronitic metatroctolite; Granulite facies; Moldanubian Zone; Sapphirine; Spinel; Variscan orogeny

Indexed keywords

BINARY ALLOYS; CORUNDUM; FELDSPAR; GARNETS; GEOCHRONOLOGY; IGNEOUS ROCKS; LEAD ALLOYS; MAGNESITE; OLIVINE; SERPENTINE; STRUCTURAL GEOLOGY; TEXTURES; ZIRCON;

CORONITIC METATROCTOLITE; GRANULITE FACIES; MOLDANUBIAN ZONES; SAPPHIRINE; SPINEL; VARISCAN OROGENIES;

METAMORPHIC ROCKS;

CORONA; GRANULITE FACIES; HERCYNIAN OROGENY; HIGH PRESSURE; ORTHOPYROXENE; OVERPRINTING; SAPPHIRINE; SPINEL; ULTRAHIGH PRESSURE METAMORPHISM;

BOHEMIAN MASSIF;

EID: 84924334045     PISSN: 02634929     EISSN: 15251314     Source Type: Journal    
DOI: 10.1111/jmg.12121     Document Type: Article

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