The terrestrial Paleocene sequences at the north of Ankara are chiefly composed of alluvial fan deposits, braided and meandering river sediments and lacustrine carbonate mudstones. In a limited area, only around Orhaniye village, fine-grained volcanoclastics and lavaş are observed. Ali these deposits are in a vertical örder both grain size and depositional environment and they pass into marine Eocene units.
| Primary Language | English | 
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| Subjects | Structural Biology | 
| Journal Section | Research Articles | 
| Authors | |
| Publication Date | January 1, 1986 | 
| Published in Issue | Year 1986 Volume: 04 (1986) Issue: 01.02 | 
Communications Faculty of Sciences University of Ankara Series C Biology licensed under a Creative Commons Attribution 4.0 International License.