Tectonostratigraphic relationships between the North Anatolian Thrust Zone (NATZ), and the Kirsehir Massif to the north of Sivas (Turkey)

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Atıf İçin Kopyala

ÖZDEN S., Poisson A., Ozturk A., Bellier J., Blondeau A., Wernli R., ...Daha Fazla

COMPTES RENDUS DE L ACADEMIE DES SCIENCES SERIE II FASCICULE A-SCIENCES DE LA TERRE ET DES PLANETES, cilt.327, sa.10, ss.705-711, 1998 (SCI-Expanded)

• Yayın Türü: Makale / Tam Makale
• Cilt numarası: 327 Sayı: 10
• Basım Tarihi: 1998
• Doi Numarası: 10.1016/s1251-8050(99)80029-9
• Dergi Adı: COMPTES RENDUS DE L ACADEMIE DES SCIENCES SERIE II FASCICULE A-SCIENCES DE LA TERRE ET DES PLANETES
• Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
• Sayfa Sayıları: ss.705-711
• Çanakkale Onsekiz Mart Üniversitesi Adresli: Evet

Özet

In Central Anatolia, to the north of Sivas, the remains of the Northern Neotethyan domain crops out in a system of south verging th rust slices intercalated between the Eurasiatic margin (Tokat Massif), and the Taurus. In these nappes, sedimentary sequences have recorded the last steps of the Neotethyan evolution during the Late Cretaceous and of its closure during Palaeogene times. An ophiolitic melange is dated as Cenomano-Turonian or older and the thrusting of the Neotethyan nappes onto the Taurus belt (which corresponds to the closure of the Neotethys), is pre-Cuisian. ((C) Academie des sciences / Elsevier, Paris.).