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Determination of structural characteristics of Tuzgölü Fault Zone using gravity and magnetic methods, Central Anatolia

Yıl 2020, Cilt: 162 Sayı: 162, 145 - 174, 15.08.2020
https://doi.org/10.19111/bulletinofmre.661245

Öz

The anomaly maps and amplitude and wavelength changes of the anomalies obtained from gravity and magnetic methods can provide to identify fault traces in the underground. The Tuzgölü Fault Zone (TFZ), the NW-SE striking active fault zone in central Anatolia, includes fault strands that cut the basement and basin deposits. Our magnetic and gravity analysis suggests that Tuzgölü Basin and its surroundings are characterized by distinct depression and ridge areas. Gravity anomaly data show the presence of faults at depths of sea level (0 m), -1000 m, -2000 m, -3000 m, and -4000 m. These faults are mostly normal and reverse faults, as well as the lesser amount of vertical faults (high-angle normal/reverse faults) with NW-SE, N-S, and NE-SW-striking. The normal faults are of the structural development and the deposition of the Tuzgölü Basin units, which occurred late Cretaceous-Middle Eocene and Early Miocene-Quaternary Periods. The reverse faults originated from the result of the regional-scale compressional regime during Middle Eocene-Late Oligocene/ Early Miocene based on the fault dating data from the literature. The active TFZ, including several fault strands, are relatively younger faults in the region that have initiated to develop during faulting events from after Middle Miocene or Early Pliocene.

Teşekkür

Dr. Ayşe Çağlayan and Reza Saber are thanked for scientific discussion, useful suggestions, and their substantial advice during manuscript preparation. The authors also sincerely thank Prof. Dr. Bora Rojay, Sait Yüksel, Prof. Dr. Nurettin Kaymakçı, and the anonymous reviewers for their constructive and critical comments on an earlier version of this manuscript.

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Yıl 2020, Cilt: 162 Sayı: 162, 145 - 174, 15.08.2020
https://doi.org/10.19111/bulletinofmre.661245

Öz

Kaynakça

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  • Işık, V. 2009. Ductile shear zone in granitoid of Central Anatolian Crystalline Complex, Turkey: Implications for Late Cretaceous extensional deformation. Journal of Asian Earth Science 34, 507-521.
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  • Köksal, S., Romer, R.L., Göncüoğlu, M.C., Toksoy-Köksal,F. 2004. Timing of post-collision H-type to A-type granitic magmatism: U-Pb titanite ages from the Alpine central Anatolian granitoids Turkey. International Journal of Earth Sciences 93, 974- 989.
  • Kürçer, A. 2012. Tuz Gölü Fay Zonu’nun Neotektonik Özellikleri ve Paleosismolojisi, Orta Anadolu, Türkiye. Doktora Tezi, Ankara Üniversitesi, 318 sayfa, Ankara (unpublished).
  • Kürçer, A., Gökten, Y. 2014. Neotectonic-Period Characteristics, Seismicity, Geometry And Segmentation Of The Tuz Gölü Fault Zone. Bulletin of the Mineral Research and Exploration 149, 19-69.
  • Lefebvre, C., Barnhoorn, A., Van Hinsbergen, D.J.J., Kaymakçı, N., Vissers, R.L.M. 2011. Late Cretaceous extensional denudation along a marble detachment fault zone in the Kırşehir massif near Kaman, central Turkey. Journal Structural Geology 33, 1220-1236.
  • Lefebvre, C., Meijers, M.J.M., Kaymakçı, N., Peynircioğlu, A., Langereis, C. G., Van Hinsbergen, D.J.J. 2013. Reconstructing the geometry of central Anatolia during the late Cretaceous: Large-scale Cenozoic rotations and deformation between the Pontides and Taurides. Earth and Planetary Science Letters 366, 83-98.
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  • Lyatsky, H., Dietrich, J. 1998. Mapping Precambrien Basement Structure Beneath The Williston Basin in Canada: Insights From Horizontal-Gradient Vector Processing of Gravity and Magnetic Data. Canadian Journal of Exploration Geophysics 34 (1&2), 40-48.
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  • Nairn, S.P., Robertson, A.H.F., Ünlügenç, U.C., Taşlı, K, İnan, N. 2013. Tectonostratigraphic evolution of the Upper Cretaceous-Cenozoic central Anatolian basins: an integrated study of diachronous ocean basin closure and continental collision. Geological Development of Anatolia and the Easternmost Mediterranean Region. Geological Society, London Special Publication 372, 343-384.
  • Naumann, E. 1896. Die Grundlinien Anatoliens und Centralasiens. Geographische Zeitschrift 2(1), 7-25.
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  • Oruç, B. 2013. Yeraltı Kaynak Aramalarında Gravite Yöntemi. Umuttepe Yayınları 270, Kocaeli.
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  • Özsayın, E., Çiner, A., Rojay, B., Dirik, K., Melnick, D., Fernando-Blanco, D., Sudo, M. 2013. Plio- Quaternary extensional tectonics of the Central Anatolian Plateau: A case study from the Tuz Gölü Basin, Turkey. Turkish Journal of Earth Science 22,5, 691-714.
  • Pınar, R. 1984. Potansiyel Alanlarda Yukarı ve Aşağı Analitik Uzanımlar. Bilimsel Madencilik Dergisi 23(2), 5-18.
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  • Platzman, E. S., Tapırdamaz, C., Sanver, M. 1998. Neogene anticlockwise rotation of central Anatolia (Turkey): Preliminary paleomagnetic and geochronological results. Tectonophysics 299, 175–189.
  • Poisson, A., Guezou, J.C., Öztürk, A., Inan, S., Temiz, H., Gürsoy, H., Kavak, K.S., Özden, S. 1996. Tectonic setting and evolution of the Sivas basin. International Geology Review 38, 833-853.
  • Reynolds, J.M. 2011. An Introduction to Applied and Environmental Geophysics, 2nd Edition. Wiley&Blackwell 710 p.
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  • Roest, W., Verhoef, J., Pilkington, M. 1992. Magnetic Interpretation Using The 3-D analytic signal. Geophysics 57(1), 116-125.
  • Rojay, B. 2013. Tectonic evolution of the Cretaceous Ankara Ophiolitic Mélange during the Late Cretaceous to pre-Miocene interval in Central Anatolia, Turkey. Journal of Geodynamics 65, 66-81.
  • Saad, A. 2006. Understanding gravity gradients a tutorial. The Leading Edge 25(8), 942-949.
  • Salem, A., Williams, S., Fairhead, D., Smith, R., Ravat, D. 2008. Interpretation of magnetic data using tilt- angle derivatives. Geophysics 73(1), 14JF-Z11.
  • Schmitt, A.K., Danışık, M., Aydar, E., Şen, E., Ulusoy, İ., Lovera, O.M. 2014. Identifying the Volcanic Eruption Depicted in a Neolithic Painting at Çatalhöyük, Central Anatolia, Turkey. PLOS ONE 9(1): e84711.
  • Seyitoğlu, G., Kazancı, N., Karadenizli, L., Şen, Ş., Varol, B., Karabıyıkoğlu, T. 2000. Rockfall avalanche deposits associated with normal faulting in the NW of Çankırı basin: implication for the post- collisional tectonic evolution of the Neo-Tethyan suture zone. Terra Nova 12, 245-251.
  • Seyitoğlu, G., Işık, V., Gürbüz, E., Gürbüz, A. 2017. The discovery of a low-angle normal fault in the Taurus Mountains the İvriz detachment and implications concerning the Cenozoic geology of southern Turkey. Turkish Journal of Earth Sciences 26, 189-205.
  • Seymen, İ. 1984. Kırşehir masifi metamorfitlerinin jeoloji evrimi. Ketin Sempozyumu, Türkiye Jeoloji Kurumu Yayını 133-48.
  • Soengkono, S. 1999. Te Kopia geothermal system (New Zeland)-the relationship between its structure and extent. Geothermics 28(6), 767-784.
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  • Toprak, V., Göncüoğlu, M.C. 1993. Tectonic control on the development of the Neogene-Quaternary Central Anatolian Volcanic Province, Turkey. Geological Journal 28, 357-369.
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  • Tüysüz, O., Dellaloğlu, A.A., Terzioğlu, N. 1995. A magmatic belt within the Neo-Tethyan suture zone and its role in the tectonic evolution of northern Turkey. Tectonophysics 243, 173–191.
  • Uğurtaş, G. 1975. Geophysical Interpretation of Part of The Tuz Gölü Basin. Bulletin of the Mineral Research and Exploration 85, 38-45.
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  • Uygun, A., Yaşar, M., Erkan, M., Baş, H., Çelik, E., Aygün, M., Ayok, F. 1982. Tuzgölü havzası projesi, Cilt 2. Maden Tetkik ve Arama Genel Müdürlüğü Rapor No:6859, Ankara, (unpublished).
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  • Verduzco, B., Fairhead, J.D., Green, C.M., Mackenzie, C. 2004. New insights into magnetic derivatives for structural mapping. The Leading Edge 23(2), 116- 119.
  • Whitney, D.L., Teyssier, C., Dilek, Y., Fayon, A.K. 2001. Metamorphism of the Central Anatolian Crystalline Complex, Turkey: influence of orogen-normal collision vs wrench-dominated tectonics on P-T-t paths. Journal of Metamorphic Geology 19, 411-432.
  • Wilcox, L. 1974. An analysis of Gravity Prediction Methods For Continental Areas. Defense Mapping Agency Aerospace Center, Publication No. 74-001.
  • Yalınız, M.K., Floyd, P.A., Göncüoğlu, M.C. 2000. Petrology and geotectonic significance of plagiogranite from the Sarikaraman ophiolite (Central Anatolia, Turkey). Ofioliti 25, 31-37.
  • Yıldırım, C. 2014. Relative tectonic activity assessment of the Tuz Gölü Fault Zone; Central Anatolia, Turkey. Tectonophysics 630, 183-192.
  • Yüksel, S. 2011. Petrol Aramacılığında Doğal Potansiyel Yöntemler Gravite ve Manyetik. TPAO Kurum İçi Eğitim Notları 231 s.
  • Yürür, M.T., Genç, Y. 2006. The Savcili thrust fault (Kirsehir region, central Anatolia): a backthrust fault, a suture zone or a secondary fracture in an extensional regime? Geological Carpathica 57, 47-56.
  • Zhang, H., Tian-You, L., Yu-Shan, Y. 2011. Calculation of gravity and magnetic source boundaries based on anisotropy normalized variance. Chinese Journal of Geophysics 54(4), 560-567.
Toplam 112 adet kaynakça vardır.

Ayrıntılar

Birincil Dil İngilizce
Konular Mühendislik
Bölüm Makaleler
Yazarlar

Bahar Dinçer Bu kişi benim 0000-0001-6855-8084

Veysel Işık 0000-0003-0296-8237

Yayımlanma Tarihi 15 Ağustos 2020
Yayımlandığı Sayı Yıl 2020 Cilt: 162 Sayı: 162

Kaynak Göster

APA Dinçer, B., & Işık, V. (2020). Determination of structural characteristics of Tuzgölü Fault Zone using gravity and magnetic methods, Central Anatolia. Bulletin of the Mineral Research and Exploration, 162(162), 145-174. https://doi.org/10.19111/bulletinofmre.661245
AMA Dinçer B, Işık V. Determination of structural characteristics of Tuzgölü Fault Zone using gravity and magnetic methods, Central Anatolia. Bull.Min.Res.Exp. Ağustos 2020;162(162):145-174. doi:10.19111/bulletinofmre.661245
Chicago Dinçer, Bahar, ve Veysel Işık. “Determination of Structural Characteristics of Tuzgölü Fault Zone Using Gravity and Magnetic Methods, Central Anatolia”. Bulletin of the Mineral Research and Exploration 162, sy. 162 (Ağustos 2020): 145-74. https://doi.org/10.19111/bulletinofmre.661245.
EndNote Dinçer B, Işık V (01 Ağustos 2020) Determination of structural characteristics of Tuzgölü Fault Zone using gravity and magnetic methods, Central Anatolia. Bulletin of the Mineral Research and Exploration 162 162 145–174.
IEEE B. Dinçer ve V. Işık, “Determination of structural characteristics of Tuzgölü Fault Zone using gravity and magnetic methods, Central Anatolia”, Bull.Min.Res.Exp., c. 162, sy. 162, ss. 145–174, 2020, doi: 10.19111/bulletinofmre.661245.
ISNAD Dinçer, Bahar - Işık, Veysel. “Determination of Structural Characteristics of Tuzgölü Fault Zone Using Gravity and Magnetic Methods, Central Anatolia”. Bulletin of the Mineral Research and Exploration 162/162 (Ağustos 2020), 145-174. https://doi.org/10.19111/bulletinofmre.661245.
JAMA Dinçer B, Işık V. Determination of structural characteristics of Tuzgölü Fault Zone using gravity and magnetic methods, Central Anatolia. Bull.Min.Res.Exp. 2020;162:145–174.
MLA Dinçer, Bahar ve Veysel Işık. “Determination of Structural Characteristics of Tuzgölü Fault Zone Using Gravity and Magnetic Methods, Central Anatolia”. Bulletin of the Mineral Research and Exploration, c. 162, sy. 162, 2020, ss. 145-74, doi:10.19111/bulletinofmre.661245.
Vancouver Dinçer B, Işık V. Determination of structural characteristics of Tuzgölü Fault Zone using gravity and magnetic methods, Central Anatolia. Bull.Min.Res.Exp. 2020;162(162):145-74.

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