On the occurrence of primary dolomites in Qatrani Formation (Oligocene) in Fayoum Province, Western Desert, Egypt
This work represents a study of pétrographie properties, differential thermal analysis and лг-ray diffraction study of carbonate rocks of the Qatrani formation of Oligocene age in Fayoum Province, Egypt. These carbonate rocks can be grouped into three major textural and compositional types. Microcry...
Elmentve itt :
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| Dokumentumtípus: | Cikk |
| Megjelent: |
University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Szeged
1975
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| Sorozat: | Acta mineralogica-petrographica
22 No. 1 |
| Kulcsszavak: | Kőzettan, Ásványtan, Földtan |
| Tárgyszavak: | |
| Online Access: | http://acta.bibl.u-szeged.hu/24592 |
| Tartalmi kivonat: | This work represents a study of pétrographie properties, differential thermal analysis and лг-ray diffraction study of carbonate rocks of the Qatrani formation of Oligocene age in Fayoum Province, Egypt. These carbonate rocks can be grouped into three major textural and compositional types. Microcrystalline dolostones or dolomicrite, gypsiferous dolomicrite and dolomitic sandstones. |
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| Terjedelem/Fizikai jellemzők: | 119-131 |
| ISSN: | 0365-8066 |