2D modelling the depth of the southeastern Thrace Basin by using Bouguer gravity anomalies
Author:
Funder
Bilimsel Araştirma Projeleri Birimi, Istanbul Üniversitesi
Publisher
Springer Science and Business Media LLC
Subject
Geophysics
Link
https://link.springer.com/content/pdf/10.1007/s11600-023-01140-2.pdf
Reference50 articles.
1. Abdelsalam MG, Dawoud AS (1991) The Kabus Ophiolitic Melange, Sudan, and its bearing on the western boundary of the Nubian shield. J Geol Soc 148(1):83–92. https://doi.org/10.1144/gsjgs.148.1.0083
2. Akgündüz S, Koral H (2021) Paleogene extension in the Northern Aegean: colluvial/debris flow deposits of the early–middle Eocene in the NW Thrace Basin Turkey. Geol Carpath 72(3):213–231. https://doi.org/10.31577/GEOLCARP.72.3.3
3. Aral İF (2004) Karatepe Bazaltlarının (Çorlu-Tekirdağ) Yapı Malzemesi Olarak Kullanılabilirliği. İstanbul Üniversitesi Mühendislik Fakültesi Yerbilimleri Dergisi 17(2):69–76
4. Atalık E (1992) Depositional systems of the Osmancýk formation in the Thrace Basin. Middle East Technical University
5. Burke WE, Uğurtaş G (1974) Seismic interpretation of the Thrace Basin. II. Turkish Congress of Petroleum
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