Acta Geologica 32. (1989)
1-2. szám - G. Császár: Transgressive Urgonian sequence with black "pebbles" from the Villány Mountains, Hungary
URGONIAN SEQUENCE meter thickness and of varied structure of the Villány imbrication bauxitic clay is found (Császár, G., Farkas, L., 1982). In this paper some results on the unique sequence of the Nagyharsány quarry belonging to the latter imbrication will be reported first of all from paleoenvironmental and sedimentological points of view. Fig. 2. Structural sketch and Cretaceous formations of the Villány Mountains. (Used maps: Fülöp, I., 1966; Nagy, E., 1976.) 1. Bisse Marl Formation; 2. Nagyharsány Limestone Formation; 3. Harsányhegy Bauxite Formation; 4. Jurassic formations; 5. Triassic formations; 6. Paleozoic and metamorphic formations; 7. Mesozoic formations on the surface; 8. overthrust (imbrication); 9. fault