Palaeozoic and Precambrian formations of the area of Algyő, Ferencszállás and Kiskundorozsma, Hungary

T. Kovács Gábor: Palaeozoic and Precambrian formations of the area of Algyő, Ferencszállás and Kiskundorozsma, Hungary. In: Acta mineralogica-petrographica, (23) 2. pp. 267-278. (1978)

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Abstract

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 Algyő—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, Algyő) and by the pegmatite and granite porphyre dykes penetrating the metamorphites (Ferencszállás).

Item Type: Article
Journal or Publication Title: Acta mineralogica-petrographica
Date: 1978
Volume: 23
Number: 2
ISSN: 0365-8066
Page Range: pp. 267-278
Language: English
Publisher: University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Place of Publication: Szeged
Related URLs: http://acta.bibl.u-szeged.hu/39397/
Uncontrolled Keywords: Kőzettan, Ásványtan, Földtan
Additional Information: Bibliogr.: p. 277-278. ; ill. ; összefoglalás angol nyelven
Subjects: 01. Natural sciences
01. Natural sciences > 01.05. Earth and related environmental sciences
Date Deposited: 2016. Oct. 17. 09:25
Last Modified: 2022. Jul. 25. 11:01
URI: http://acta.bibl.u-szeged.hu/id/eprint/24634

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