The sklené garnet peridotite: Petrology, geochemistry, and structure of a mantle-derived boudin in Moldanubian granulite

Journal of Geosciences

Volumn 54, Issue 4, 2009, Pages 301-323

  Medaris Jr , Gordon ^a   Ackerman, Lukáš ^b,c   Jelínek, Emil ^d   Toy, Virginia ^e   Siebel, Wolfgang ^f   Tikoff, Basil ^a  

^a UNIVERSITY OF WISCONSIN MADISON   (United States)

^b INSTITUTE OF GEOLOGY   (Czech Republic)

^c CZECH GEOLOGICAL SURVEY   (Czech Republic)

^d CHARLES UNIVERSITY   (Czech Republic)

^e UNIVERSITY OF OTAGO   (New Zealand)

^f UNIVERSITY OF TÜBINGEN   (Germany)

Author keywords

Geochemistry; LPO; Moldanubian; Peridotite; Pt conditions; Radiogenic isotopes

Indexed keywords

ENTRAINMENT; GARNET; GRAIN SIZE; GRANULITE; IGNEOUS GEOCHEMISTRY; LATTICE DYNAMICS; MANTLE PROCESS; MANTLE SOURCE; MINERAL; P-T CONDITIONS; PERIDOTITE; PETROLOGY; PORPHYROBLAST; PREFERRED ORIENTATION; RECRYSTALLIZATION; BOUDINAGE; CLINOPYROXENE; LITHOSPHERIC STRUCTURE; OLIVINE; ORTHOPYROXENE; PETROGENESIS; RARE EARTH ELEMENT;

BRUNIA;

EID: 76349122759     PISSN: 18026222     EISSN: None     Source Type: Journal    
DOI: 10.3190/jgeosci.052     Document Type: Article

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