Geodynamic implications of flattened tabular equigranular textured peridotites from the Bakony-Balaton Highland Volcanic Field (Western Hungary)

Journal of Geodynamics

Volumn 43, Issue 4-5, 2007, Pages 484-503

  Hidas, Károly ^a   Falus, György ^a,b   Szabó, Csaba ^a   Szabó, Péter János ^c   Kovács, István ^a,d   Földes, Tamás ^e  

^a EÖTVÖS LORÁND UNIVERSITY   (Hungary)

^b GEOLOGICAL AND GEOPHYSICAL INSTITUTE OF HUNGARY   (Hungary)

^c BUDAPEST UNIVERSITY OF TECHNOLOGY AND ECONOMICS   (Hungary)

^d AUSTRALIAN NATIONAL UNIVERSITY   (Australia)

^e SZENT ISTVÁN UNIVERSITY   (Hungary)

Author keywords

Bakony Balaton Highland Volcanic Field; Carpathian Pannonian Region; Crystallographic preferred orientation (CPO); EBSD; Flattened tabular equigranular texture; Peridotite xenoliths

Indexed keywords

BASALT; CRYSTALLOGRAPHY; DEFORMATION MECHANISM; GEODYNAMICS; LITHOSPHERIC STRUCTURE; OLIVINE; ORTHOPYROXENE; PERIDOTITE; TECTONIC EVOLUTION; TEXTURE; UPPER MANTLE; XENOLITH;

CARPATHIANS; CENTRAL EUROPE; EURASIA; EUROPE; HUNGARY;

EID: 34247248350     PISSN: 02643707     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jog.2006.10.007     Document Type: Article

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