In ıhe investigated area successive deformations are exhibiıed in the Upper Creta- ceous-Miocene series due to the subduction and Continental collision in the Northern branch of Ncotethys. Four deformational stages (D 1-4) can be recognized in the series, the first two (Dİ—2) of which may represent the independent events. The main deformation (D3) takes place towards the end of Mid-Miocene time in this period due to Continental collision, Last stage affected the previous struetures as the late events of D3. The tectonic îinaments of the region extend in NE-SW and NW-SE direetions.
Birincil Dil | İngilizce |
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Konular | Yapısal Biyoloji |
Bölüm | Research Article |
Yazarlar | |
Yayımlanma Tarihi | 1 Ocak 1986 |
Yayımlandığı Sayı | Yıl 1986 Cilt: 04 (1986) Sayı: 01.02 |
Communications Faculty of Sciences University of Ankara Series C-Biology.
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