These structures take up the internal deformation of the Anatolian Plate.
📌 3 Maddede Bu Makale
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Amaç & Hipotez:This paper suggests that the structure known as "Beypazarı flexure / monocline" in the Turkish geology literature should be named as "Beypazarı fault-propagation folds".
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Temel Bulgular & Veri:Beypazarı, Kilci and Başören blind thrusts together with Erenler back thrust constitute the Beypazarı Blind Thrust Zone which is an active neotectonic structure as indicated by earthquake activity.
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Sonuç & Katkı:These structures take up the internal deformation of the Anatolian Plate.
This paper suggests that the structure known as "Beypazarı flexure / monocline" in the Turkish geology literature should be named as "Beypazarı fault-propagation folds". Beypazarı, Kilci and Başören blind thrusts together with Erenler back thrust constitute the Beypazarı Blind Thrust Zone which is an active neotectonic structure as indicated by earthquake activity. NW-SE contraction created by the interaction between the North Anatolian Fault Zone, the Kırıkkale-Erbaa Fault Zone and the Eskişehir Fault Zone produced the Eldivan-Elmadağ Pinched Crustal Wedge, the Abdüsselam Pinched Crustal Wedge and the Beypazarı Blind Thrust Zone. These structures take up the internal deformation of the Anatolian Plate.
SEYİTOĞLU, G., ESAT, K., KAYPAK, B. (2017). ONE OF THE MAIN NEOTECTONIC STRUCTURES IN THE NW CENTRAL ANATOLIA: BEYPAZARI BLIND THRUST ZONE AND RELATED FAULT-PROPAGATION FOLDS. Maden Tetkik ve Arama Dergisi, Cilt: 154 - Sayı: 154, 1–14. https://ajindex.com/articles/53980
Aksoy, C.O., Onargan, T., Yenice, H., Küçük; K., Köse, H. 2006. Determining the stress and convergence at Beypazarı trona field by three- dimensional elastic-plastic finite element analysis: A case study. International Journal of Rock Mechanics and Mining Sciences, 43, 166-178.
Allmendinger, R.W. 1998. Inverse and forward numerical modeling of trishear fault-propagation folds. Tectonics, 17, 640-656.
Apaydın, A. 2010. Relation of tectonic structure to groundwater flow in the Beypazarı region, NW Anatolia, Turkey. Hydrogeology Journal, 18, 1343-1356.
Bechtel, A., Karayiğit, A.İ., Sachsenhofer, R.F., İnaner, H., Christanis, K., Gratzer, R. 2014. Spatial and temporal variability in vegetation and coal facies as reflected by organic petrological and geochemical data in the Middle Miocene Çayırhan coal field (Turkey). International Journal of Coal Geology, 134/135, 46-60.
Bürküt, Y., Suner, F., Esenli, V. 1998. Çayırhan-Beypazarı bölgesi (Ankara) Tenardit-Trona yatakları oluşum koşulları. Yerbilimleri Geosound, 32, 191-198.
Calamita, F., Pace, P., Satolli, S. 2012. Coexistence of fault-propagation and fault-bend folding in curve-shaped foreland fold-and-thrust belts: examples from the Northern Apennines (Italy). Terra Nova, 24, 396-406.
Demirci, C.Y. 2000. Structural Analysis in Beypazarı-Ayaş-Kazan-Peçenek Area, NW of Ankara (Turkey). PhD thesis Middle East Technical University. Diker, S., Çelik, M., Kadıoğlu, Y.K. 2006. Fingerprints of the formation of geothermal springs on the granitoids: Beypazarı-Ankara, Turkey. Environmental Geology, 51, 365-375.
Emre, Ö., Duman, T.Y., Özalp, S., Elmacı, H., Olgun, Ş., Şaroğlu, F. 2013. Active fault map of Turkey with an explanatory text 1:1,250,000 scale. Special Publication Series 30, General Directorate of Mineral Research and Exploration, Ankara-Turkey. ISBN: 978-605-5310-56-1
Esat, K., Kaypak, B., Işık, V., Ecevitoğlu, B., Seyitoğlu, G. 2016. The Ilıca branch of the southeastern Eskişehir Fault Zone: an active right-lateral strike-slip structure in central Anatolia, Turkey. MTA Dergisi, in press. Esat et al. in review. Abdüsselam Pinched Crustal Wedge: a Late Cenozoic structure related to the contractional regime in the NW Central Anatolia. MTA Dergisi. Esat, K. 2011. Ankara çevresinde Orta Anadolu'nun neotektoniği ve depremselliği [Neotectonics and seismicity of the central Anatolia around Ankara]. Doktora Tezi, Ankara Üniversitesi Fen Bili