The series outcropped between Bağlum and Kazan towns in the northwest of Ankara are the sandstone rich flysch
representing the interval of Late Campanian - Maestrichtian, fluvial and limnic sediments of Paleocene epoch, shallow marine
limestones of Lutetiari age, and limnic and fluvial type continental series of Late Eocene and Mid Miocene period. The only uncomformity
in the series of Late Campanian and Miocene is seen between Maestrichtian and Paleocene in the area. The continental
occurrences of Pliocene, cover the older units by an angular uncomformity. The formations representing the period of Late Campanian
and Miocene had folded together related to the continental collision commencing by Mid Miocene. The region bears the
features of a fore-arc depositional basin in the mentioned period.
Birincil Dil | İngilizce |
---|---|
Konular | Mühendislik |
Bölüm | Makaleler |
Yazarlar | |
Yayımlanma Tarihi | 1 Ocak 1988 |
Yayımlandığı Sayı | Yıl 1988 Cilt: 108 Sayı: 108 |
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