The Silurian and Devonian in the surroundings of Nekézseny (southernmost Uppony Mts, Northern Hungary)

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
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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