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.
Birincil Dil | İngilizce |
---|---|
Konular | Yapısal Biyoloji |
Bölüm | Research Article |
Yazarlar | |
Yayımlanma Tarihi | 1 Ocak 1986 |
Yayımlandığı Sayı | Yıl 1986 |
Communications Faculty of Sciences University of Ankara Series C-Biology.
This work is licensed under a Creative Commons Attribution 4.0 International License.