The internal structure of Beypazarı Blind Thrust Zone around Çayırhan

The Beypazarı Blind Thrust Zone, which is surrounded by the North Anatolian, the Eskişehir, and the Kırıkkale-Erbaa fault zones, is a recently defined neotectonic structure developed in the NW central Anatolia together with the Eldivan-Elmadağ and the Abdüsselam Pinched Crustal Wedges. In this study...

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Main Authors: Anıl Ardahanlıoğlu, Gürol Seyi̇toğlu, Korhan Esat
Format: Article
Language:English
Published: General Directorate of Mineral Research and Exploration 2020-12-01
Series:Bulletin of the Mineral Research and Exploration
Subjects:
Online Access:https://dergipark.org.tr/tr/pub/bulletinofmre/issue/54946/651712?publisher=mta
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spelling doaj-7f88556f9b7a4c5ba03df80f9c402b0f2020-12-17T14:24:53ZengGeneral Directorate of Mineral Research and ExplorationBulletin of the Mineral Research and Exploration0026-45632020-12-01163163779710.19111/bulletinofmre.65171276The internal structure of Beypazarı Blind Thrust Zone around ÇayırhanAnıl ArdahanlıoğluGürol Seyi̇toğluKorhan EsatThe Beypazarı Blind Thrust Zone, which is surrounded by the North Anatolian, the Eskişehir, and the Kırıkkale-Erbaa fault zones, is a recently defined neotectonic structure developed in the NW central Anatolia together with the Eldivan-Elmadağ and the Abdüsselam Pinched Crustal Wedges. In this study, the internal structure of the Beypazarı Blind Thrust Zone has been examined in detail around Çayırhan region. It has been defined that it consists of the Karaköy, Sekli, Nalçabayırı, Uzunbayır blind thrusts, Davutoğlan Back Thrust, and Beypazarı Blind Thrust I-II from North to south, respectively with help of the fault-propagation folds in the study area. The existence of economically important and operational resources such as lignite and trona in the Neogene sequence affected by these faults in the region and earthquake generating potential of the faults determined in previous studies increase the importance of this study.https://dergipark.org.tr/tr/pub/bulletinofmre/issue/54946/651712?publisher=mtacentral anatolianeotectonicsblind thrust faultearthquakefaultpropagation fold
collection DOAJ
language English
format Article
sources DOAJ
author Anıl Ardahanlıoğlu
Gürol Seyi̇toğlu
Korhan Esat
spellingShingle Anıl Ardahanlıoğlu
Gürol Seyi̇toğlu
Korhan Esat
The internal structure of Beypazarı Blind Thrust Zone around Çayırhan
Bulletin of the Mineral Research and Exploration
central anatolia
neotectonics
blind thrust fault
earthquake
faultpropagation fold
author_facet Anıl Ardahanlıoğlu
Gürol Seyi̇toğlu
Korhan Esat
author_sort Anıl Ardahanlıoğlu
title The internal structure of Beypazarı Blind Thrust Zone around Çayırhan
title_short The internal structure of Beypazarı Blind Thrust Zone around Çayırhan
title_full The internal structure of Beypazarı Blind Thrust Zone around Çayırhan
title_fullStr The internal structure of Beypazarı Blind Thrust Zone around Çayırhan
title_full_unstemmed The internal structure of Beypazarı Blind Thrust Zone around Çayırhan
title_sort internal structure of beypazarı blind thrust zone around çayırhan
publisher General Directorate of Mineral Research and Exploration
series Bulletin of the Mineral Research and Exploration
issn 0026-4563
publishDate 2020-12-01
description The Beypazarı Blind Thrust Zone, which is surrounded by the North Anatolian, the Eskişehir, and the Kırıkkale-Erbaa fault zones, is a recently defined neotectonic structure developed in the NW central Anatolia together with the Eldivan-Elmadağ and the Abdüsselam Pinched Crustal Wedges. In this study, the internal structure of the Beypazarı Blind Thrust Zone has been examined in detail around Çayırhan region. It has been defined that it consists of the Karaköy, Sekli, Nalçabayırı, Uzunbayır blind thrusts, Davutoğlan Back Thrust, and Beypazarı Blind Thrust I-II from North to south, respectively with help of the fault-propagation folds in the study area. The existence of economically important and operational resources such as lignite and trona in the Neogene sequence affected by these faults in the region and earthquake generating potential of the faults determined in previous studies increase the importance of this study.
topic central anatolia
neotectonics
blind thrust fault
earthquake
faultpropagation fold
url https://dergipark.org.tr/tr/pub/bulletinofmre/issue/54946/651712?publisher=mta
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