Subvolcanic basaltic dyke from Beremend, Southeast Transdanubia, Hungary
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 charact...
Elmentve itt :
| Szerzők: | |
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| Dokumentumtípus: | Cikk |
| Megjelent: |
University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Szeged
1996
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| Sorozat: | Acta mineralogica-petrographica
37 |
| Kulcsszavak: | Kőzettan, Ásványtan, Földtan |
| Tárgyszavak: | |
| Online Access: | http://acta.bibl.u-szeged.hu/24842 |
| Tartalmi kivonat: | 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. |
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| Terjedelem/Fizikai jellemzők: | 181-187 |
| ISSN: | 0365-8066 |