Balogh Károly and Kozur Heinz: The Silurian and Devonian in the surroundings of Nekézseny (southernmost Uppony Mts, Northern Hungary). In: Acta mineralogica-petrographica, (27). pp. 193-205. (1985)
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Abstract
The athrogenic and volcanic sequence (Strázsahegy Formation) of the Strázsa-hegy section, at first regarded as Middle Triassic and later assumed to be Lower Devonian (Lochkovian), could be placed into the Middle Devonian. From olistolites within the tuffitic parts of this formation a complete highly fossiliferous Silurian sequence (similar to the Silurian of the Cellon section in the Carnic Alps, and consisting mainly of pelagic micritic limestones, among these also nautiloid limestones) could be reconstructed. The geological evolution of the UpponyMts from the Upper Ordovician up to the Bashkirian (Middle Carboniferous) is briefly discussed (Fig. 1 and 2).
Item Type: | Article |
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Journal or Publication Title: | Acta mineralogica-petrographica |
Date: | 1985 |
Volume: | 27 |
ISSN: | 0365-8066 |
Page Range: | pp. 193-205 |
Language: | English |
Publisher: | University of Szeged, Department of Mineralogy, Geochemistry and Petrology |
Place of Publication: | Szeged |
Related URLs: | http://acta.bibl.u-szeged.hu/39405/ |
Uncontrolled Keywords: | Kőzettan, Ásványtan, Földtan |
Additional Information: | Bibliogr.: p. 201-202. ; 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. 26. 10:00 |
URI: | http://acta.bibl.u-szeged.hu/id/eprint/24741 |
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