Subvolcanic basaltic dyke from Beremend, Southeast Transdanubia, Hungary

Molnár Sándor and Szederkényi Tibor: Subvolcanic basaltic dyke from Beremend, Southeast Transdanubia, Hungary. In: Acta mineralogica-petrographica, (37). pp. 181-187. (1996)

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Abstract

Penetrating Aptian limestones (Nagyharsany Limestone Formation) a narrow subvolcanic body (dyke) has been found in the quarry of Beremend Cement-Plant. Based on its bulk composition this rock can be ranged into the basalt group in general and its low alkaline content suggests a picrobasaltic character. K/Ar age determination (from the whole rock) show a Late Cretaceous subvolcanic event, but the petrochemical data suggest a conection with Miocene basalts and andesito-basalts from Podravska Slatina and Popovac Hill.

Item Type: Article
Journal or Publication Title: Acta mineralogica-petrographica
Date: 1996
Volume: 37
ISSN: 0365-8066
Page Range: pp. 181-187
Language: English
Publisher: University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Place of Publication: Szeged
Related URLs: http://acta.bibl.u-szeged.hu/39415/
Uncontrolled Keywords: Kőzettan, Ásványtan, Földtan
Additional Information: Bibliogr.: 187. p. ; 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. 27. 11:58
URI: http://acta.bibl.u-szeged.hu/id/eprint/24842

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