Magnetic fabrics in garnet peridotites-pyroxenites and host felsic granulites in the South Bohemian Granulites (Czech Republic): Implications for distinguishing between primary and metamorphism induced fabrics

Gondwana Research

Volumn 23, Issue 3, 2013, Pages 956-972

  Hrouda, F ^a,b   Faryad, S W ^b   Franek J ^c   Chlupacova M ^a  

^a Advanced Geoscience Instruments Company   (Czech Republic)

^b CHARLES UNIVERSITY   (Czech Republic)

^c CZECH GEOLOGICAL SURVEY   (Czech Republic)

Author keywords

Fabric relationship; Felsic granulite; Magnetic anisotropy; Mantle rock enclaves; Petrology

Indexed keywords

AMPHIBOLITE FACIES; FELSIC ROCK; GARNET; GRANULITE; MAGNETIC ANISOTROPY; MAGNETIC FABRIC; PERIDOTITE; PYROXENITE; RETROGRADE METAMORPHISM;

CZECH REPUBLIC; JIHOCESKY;

EID: 84873176497     PISSN: 1342937X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.gr.2012.05.020     Document Type: Article

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