Symplectite formation during decompression induced garnet breakdown in lower crustal mafic granulite xenoliths: Mechanisms and rates

Contributions to Mineralogy and Petrology

Volumn 159, Issue 3, 2010, Pages 293-314

  Dégi, Júlia ^a,b   Abart, Rainer ^c   Török, Kálmán ^b,d   Bali, Eniko ^e   Wirth, Richard ^f   Rhede, Dieter ^f  

^a INSTITUTE OF EXPERIMENTAL MEDICINE   (Hungary)

^b EÖTVÖS LORÁND UNIVERSITY   (Hungary)

^c FREIE UNIVERSITÄT BERLIN   (Germany)

^d GEOLOGICAL AND GEOPHYSICAL INSTITUTE OF HUNGARY   (Hungary)

^e UNIVERSITÄT BAYREUTH   (Germany)

^f GFZ GERMAN RESEARCH CENTRE FOR GEOSCIENCES   (Germany)

Author keywords

[No Author keywords available]

Indexed keywords

ANORTHITE; DECOMPRESSION; FORMATION MECHANISM; GARNET; GEOCHEMISTRY; GRANULITE; LOWER CRUST; MAFIC ROCK; PRESSURE EFFECT; REACTION KINETICS; ROCK MICROSTRUCTURE; SPINEL; SYMPLECTITE; TEMPERATURE EFFECT; THERMODYNAMICS; TRACE ELEMENT; XENOLITH;

BALATON HIGHLAND; HUNGARY; PANNONIAN BASIN; VESZPREM;

EID: 79958188088     PISSN: 00107999     EISSN: None     Source Type: Journal    
DOI: 10.1007/s00410-009-0428-z     Document Type: Article

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