DOI
10.19076/mta.30800
Abstract
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.
Recommended Citation
SEYİTOĞLU, Gürol; ESAT, Korhan; and KAYPAK, Bülent
(2023)
"ONE OF THE MAİN NEOTECTONİC STRUCTURES İN THE NW CENTRAL ANATOLİA: BEYPAZARI BLİND THRUST ZONE AND RELATED FAULT-PROPAGATİON FOLDS,"
Bulletin of the Mineral Research and Exploration: Vol. 2017:
Iss.
154, Article 1.
DOI: https://doi.org/10.19076/mta.30800
