Palaeozoic and Precambrian formations of the area of Algyő, Ferencszállás and Kiskundorozsma, Hungary
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 o...
Elmentve itt :
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| Dokumentumtípus: | Cikk |
| Megjelent: |
University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Szeged
1978
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| Sorozat: | Acta mineralogica-petrographica
23 No. 2 |
| Kulcsszavak: | Kőzettan, Ásványtan, Földtan |
| Tárgyszavak: | |
| Online Access: | http://acta.bibl.u-szeged.hu/24634 |
| LEADER | 01926nab a2200217 i 4500 | ||
|---|---|---|---|
| 001 | acta24634 | ||
| 005 | 20220725110103.0 | ||
| 008 | 161017s1978 hu o 0|| eng d | ||
| 022 | |a 0365-8066 | ||
| 040 | |a SZTE Egyetemi Kiadványok Repozitórium |b hun | ||
| 041 | |a eng | ||
| 100 | 2 | |a T. Kovács Gábor | |
| 245 | 1 | 0 | |a Palaeozoic and Precambrian formations of the area of Algyő, Ferencszállás and Kiskundorozsma, Hungary |h [elektronikus dokumentum] / |c T. Kovács Gábor |
| 260 | |a University of Szeged, Department of Mineralogy, Geochemistry and Petrology |b Szeged |c 1978 | ||
| 300 | |a 267-278 | ||
| 490 | 0 | |a Acta mineralogica-petrographica |v 23 No. 2 | |
| 520 | 3 | |a 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). | |
| 650 | 4 | |a Természettudományok | |
| 650 | 4 | |a Föld- és kapcsolódó környezettudományok | |
| 695 | |a Kőzettan, Ásványtan, Földtan | ||
| 856 | 4 | 0 | |u http://acta.bibl.u-szeged.hu/24634/1/mineralogica_023_fasc_002_267-278.pdf |z Dokumentum-elérés |