Öz
In the eastern part of the Pasinler-Horasan Neogene basin, the lowermost section consists generally of tuffs,
andesites and basalts. This association is nomenclated as "Karakurt volcanics" They are underlain by an ophiolitic melange of
Lower Cretaceous age which is unconformably overlain by the Oligocene Çayarası formation consisting of clastic rocks. The
basin is bounded by sinistral strike-slip faults controlling sedimentation of various continental detritic rocks. These are
distinguished as Aras and Horasan formations, both Pliocene in age, representing respectively marls and claystones of deep
lagoonal environment, conformably overlain by fine grained sediments. Terrace gravels, alluvial fans and colluvium represent
the Quaternary sedimentation.
Anahtar Kelimeler
Kaynakça
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Ayrıntılar
| Birincil Dil | İngilizce |
|---|---|
| Konular | Mühendislik |
| Bölüm | Makaleler |
| Yazarlar | |
| Yayımlanma Tarihi | 1 Ağustos 1993 |
| Yayımlandığı Sayı | Yıl 1993 Cilt: 115 Sayı: 115 |
Kaynak Göster
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