The basement rocks of the investigated area, situated near Niksar, Erbaa and Destek are crossed by the Nort
Anatolian Fault they comprise Turhal group metamorphic rocks of Permo-Triassic age. It is unconformably overlain by
consisting of a sedimentary sequence of Liassic-Upper Eocene age deposited the fore-arc basin of the Eurasian continent
The study area is in the suture zone between Eurasian and Anatolian plates. Thus it is effected by a north-south compression
resulting in east-west trending thrusts in relation to formation of the North Anatolian Fault in the neotectonic period. Continental
sedimentation took place in basins during Pliocene. Later activity of the North Anatolian Fault caused formation of pull-apart
basins of Niksar, Erbaa-Taşova regions.
Birincil Dil | İngilizce |
---|---|
Konular | Mühendislik |
Bölüm | Makaleler |
Yazarlar | |
Yayımlanma Tarihi | 1 Temmuz 1992 |
Yayımlandığı Sayı | Yıl 1992 Cilt: 114 Sayı: 114 |
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