TY  - JOUR
KW  - K?zettan
KW  -  Ásványtan
KW  -  Földtan
AV  - public
N2  - In the central part of the Southern Great Plain (Szeged environment, between 1965 and 1977) about 150 hydrocarbon exploratory bores reached the metamorphic basement. The stratigraphic identification of the crystalline formations with those of the neighbouring countries shows that the metamorphites of this area are also of Precambrian origin. The Precambrian formations of the Codru Mountains can be traced probably through the Pusztaföldvár area to the Algy??Ferencszállás range (Biharia and Baia de Arie$ series). The classification of the metamorphites of Kiskundorozsma is not clear yet. The formation and stratigraphic position of the rock seems to be similar to the Some? and Baia de Arie§ series of the Bihorautochton as well as to the Lower Crystalline Sequence of the Serbo?Macedonian Massif. The Paleozoic is represented by the incompletely verified Carboniferous metamorphite breccia (Szeged, Algy?) and by the pegmatite and granite porphyre dykes penetrating the metamorphites (Ferencszállás).
ID  - acta24634
UR  - http://acta.bibl.u-szeged.hu/24634/
SP  - 267
A1  -  T. Kovács Gábor
TI  - Palaeozoic and Precambrian formations of the area of Algy?, Ferencszállás and Kiskundorozsma, Hungary
SN  - 0365-8066
VL  - 23
IS  - 2
CY  - Szeged
EP  - 278
JF  - Acta mineralogica-petrographica
N1  - Bibliogr.: p. 277-278. ; ill. ; összefoglalás angol nyelven
PB  - University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Y1  - 1978///
ER  -