Data on the geology and mineralogy of the oil shale occurrence at Pula, Hungary
The gravelly sand of basaltic and basalt tuff substance forming the basement of the oil shale and the overlying alginite was taken stratigraphically one rhythm. So the sequence overlies directly the erosion surface of the Upper Triassic dolomite. In its roof carbonate mud, humic clay and aleurite ar...
Elmentve itt :
| Szerzők: | |
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| Dokumentumtípus: | Cikk |
| Megjelent: |
University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Szeged
1976
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| Sorozat: | Acta mineralogica-petrographica
22 No. 2 |
| Kulcsszavak: | Kőzettan, Ásványtan, Földtan |
| Tárgyszavak: | |
| Online Access: | http://acta.bibl.u-szeged.hu/24601 |