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 |
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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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