Constraining the Timing of the Closure of the Intra-Pontide Ocean by U-Pb Dating of Syntectonic Calcite
TERRA NOVA, cilt.37, sa.1, ss.26-34, 2025 (SCI-Expanded, Scopus)
- Yayın Türü: Makale / Tam Makale
- Cilt numarası: 37 Sayı: 1
- Basım Tarihi: 2025
- Doi Numarası: 10.1111/ter.12743
- Dergi Adı: TERRA NOVA
- Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus, Academic Search Premier, Aquatic Science & Fisheries Abstracts (ASFA), Environment Index, Geobase, INSPEC
- Sayfa Sayıları: ss.26-34
- Anahtar Kelimeler: compressional tectonics, Neo-Tethys, oceanic closure, syntectonic calcite, U–Pb dating
- İstanbul Üniversitesi-Cerrahpaşa Adresli: Evet
Özet
The western Black Sea region is a key area for the study of the Neo-Tethys orogenic belt, as it contains records of the evolutionary history of the entire Alpine orogeny from subduction to oceanic closure and collision. The Izmir-Ankara and the Intra-Pontide suture zones represent the final closure of the Neo-Tethys oceans. However, when the final closure took place is still disputed. In this study, we investigate syn-collisional faulting events in the western Black Sea region near Istanbul. We performed kinematic analyses of faulting and U-Pb dating of syntectonic calcite precipitates on the fault planes to constrain the timing of Neo-Tethys Ocean closure and post-collisional contractional tectonics. Syntectonic calcite precipitates associated with regional N-S compressional tectonics provide precise U-Pb ages between 48 and 57 Ma, constraining the early Eocene age of reverse faulting and associated closure of the Intra-Pontide Ocean.