Preliminary petrological and geochemical studies of the area Ófalu, Mecsek Mountains, Hungary

On the northern frame of Mórágy crystalline mass near Ófalu village a detailed penological investigation was carried out in the Lower Paleozoic sequence. It is named Ófalu Phyllitoid Group dividing into three formations and seven members of alternating eugeosynclinal volcanic and sedimentary associa...

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Bibliographic Details
Main Authors: Ghoneim Mohamed Ahmed F.
Szederkényi Tibor
Format: Article
Published: University of Szeged, Department of Mineralogy, Geochemistry and Petrology Szeged 1977
Series:Acta mineralogica-petrographica 23 No. 1
Kulcsszavak:Kőzettan, Ásványtan, Földtan
Subjects:
Online Access:http://acta.bibl.u-szeged.hu/24615
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490 0 |a Acta mineralogica-petrographica  |v 23 No. 1 
520 3 |a On the northern frame of Mórágy crystalline mass near Ófalu village a detailed penological investigation was carried out in the Lower Paleozoic sequence. It is named Ófalu Phyllitoid Group dividing into three formations and seven members of alternating eugeosynclinal volcanic and sedimentary association affected a fairly low grade Abukuma type regional metamorphism produced greenschist as well as greenschist-amphibolite transition fades. The volcanism is represented by andesitic-basalt rocks with associated tuffaceous derivatives and albite-porphyry as well as serpentinized ultramafic sill-like body intruded the geosynclinal complex. According to comparative petrochemical examinations the andesitic-basalt rocks derived from oceanic type tholeiitic volcanism. 
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