Penological and geochemical character of the Bár basalt, Baranya County, South Hungary
Based on exploration carried out by deep-drillings near Bár village a small maar-like volcano covering by Quaternary loess and characterized by a sole eruption is proved. Producing a fairly well determinable thin volcanic sequence this eruption is represented by a very thin tuffaceous sheet on the b...
Elmentve itt :
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| Dokumentumtípus: | Cikk |
| Megjelent: |
University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Szeged
1980
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| Sorozat: | Acta mineralogica-petrographica
24 No. 2 |
| Kulcsszavak: | Kőzettan, Ásványtan, Földtan |
| Tárgyszavak: | |
| Online Access: | http://acta.bibl.u-szeged.hu/24656 |
| Tartalmi kivonat: | Based on exploration carried out by deep-drillings near Bár village a small maar-like volcano covering by Quaternary loess and characterized by a sole eruption is proved. Producing a fairly well determinable thin volcanic sequence this eruption is represented by a very thin tuffaceous sheet on the base of the volcanic succession and a scoria member and a porous, sometimes churned rarely compact basaltic lava mass. The basalt is classified as a leucite basanite turning into analcitebearing basanite at the margins and at some places of the porous inner sections of the volcanic body. Being a conspicuous petrologic difference between Pannonian basalts of Hungary and Bár alkaline rocks, the latter is regarded as an independent volcanic event of the great Pannonian volcanism of Hungary. |
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| Terjedelem/Fizikai jellemzők: | 235-244 |
| ISSN: | 0365-8066 |