Journals / Bulletin of the mineral research and exploration / 2020 / Cilt: 0 - Sayı: 163

The internal structure of Beypazarı Blind Thrust Zone around Çayırhan

Beypazarı Kör Bindirme Zonu’nun Çayırhan civarındaki iç yapısı

Pages
77–97
Publication Date
2022-10-12
DOI
—
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AI Summary & Key Takeaways

AI Insight
⚡ TL;DR(Too Long; Didn't Read)

The existence ofeconomically important and operational resources such as lignite and trona in the Neogene sequenceaffected by these faults in the region and earthquake generating potential of the faults determined inprevious studies increase the importance of this study.

📌 3 Key Takeaways

🎯
Objective & Hypothesis:The Beypazarı Blind Thrust Zone, which is surrounded by the North Anatolian, the Eskişehir, andthe Kırıkkale-Erbaa fault zones, is a recently defined neotectonic structure developed in the NWcentral 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 detailaround Çayırhan region.
📊
Key Findings & Data: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 northto south, respectively with help of the fault-propagation folds in the study area.
💡
Conclusion & Impact:The existence ofeconomically important and operational resources such as lignite and trona in the Neogene sequenceaffected by these faults in the region and earthquake generating potential of the faults determined inprevious studies increase the importance of this study.
🔬Design:Research Article
📍Scope:Comprehensive Sample
⚙️Variables:Domain Parameters

Abstract

The Beypazarı Blind Thrust Zone, which is surrounded by the North Anatolian, the Eskişehir, andthe Kırıkkale-Erbaa fault zones, is a recently defined neotectonic structure developed in the NWcentral 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 detailaround 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 northto south, respectively with help of the fault-propagation folds in the study area. The existence ofeconomically important and operational resources such as lignite and trona in the Neogene sequenceaffected by these faults in the region and earthquake generating potential of the faults determined inprevious studies increase the importance of this study.

Özet

Yakın zamanda tanımlanmış olan Beypazarı Kör Bindirme Zonu, KB İç Anadolu’da Kuzey Anadolu Fay Zonu, Eskişehir Fay Zonu ve Kırıkkale-Erbaa Fay Zonu arasında Eldivan-Elmadağ ve Abdüsselam kıstırılmış tektonik kamaları ile birlikte gelişen neotektonik bir yapıdır. Beypazarı Kör Bindirme Zonu’nun iç yapısı Çayırhan civarında ayrıntıları ile incelenmiş ve kuzeyden güneye doğru Karaköy, Sekli, Nalçabayırı, Uzunbayır kör bindirmeleri ile Davutoğlan Geri Bindirmesi ve Beypazarı Kör Bindirmesi I-II’den meydana geldiği fay-ilerleme kıvrımlarından da yararlanarak ortaya konmuştur. Bu faylardan etkilenen Neojen istifin içerdiği linyit ve trona gibi ekonomik değerlerin işletiliyor olması ve önceki çalışmalarda fayların deprem üretme potansiyelinin belirlenmiş olması çalışmanın önemini arttırmaktadır.

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Cite This Article

ARDAHANLIOĞLU, A., SEYİTOĞLU, G., ESAT, K. (2022). The internal structure of Beypazarı Blind Thrust Zone around Çayırhan. Bulletin of the mineral research and exploration, Cilt: 0 - Sayı: 163, 77–97. https://ajindex.com/articles/469382

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