Reduced carbonic fluids in mafic granulite xenoliths from the Bakony - Balaton Highland Volcanic Field, W-Hungary

Chemical Geology

Volumn 223, Issue 1-3, 2005, Pages 93-108

  Török, Kálmán ^a,b   Dégi, Júlia ^a   Szép, Andrea ^c   Marosi, György ^c  

^a EÖTVÖS LORÁND UNIVERSITY   (Hungary)

^b GEOLOGICAL AND GEOPHYSICAL INSTITUTE OF HUNGARY   (Hungary)

^c BUDAPEST UNIVERSITY OF TECHNOLOGY AND ECONOMICS   (Hungary)

Author keywords

CO2 CO C system; Crustal thinning; Fluid inclusion; Garnet granulite; Xenolith

Indexed keywords

CARBON; FLUID INCLUSION; GRANULITE; XENOLITH;

BAKONY MOUNTAINS; BALATON HIGHLAND; CENTRAL EUROPE; EASTERN HEMISPHERE; EURASIA; EUROPE; HUNGARY; TRANSDANUBIAN MOUNTAINS; WORLD;

EID: 28244475052     PISSN: 00092541     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.chemgeo.2005.05.010     Document Type: Article

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