Morpho-tectonic features with dextrally offset stream channels (7 km) and ground ruptures of the 1943 Ladik-Ilgaz earthquake of M 7.2 strongly suggest that the first fault system is an active right lateral strike-slip fault zone
📌 3 Key Takeaways
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Objective & Hypothesis:The Beşpınar-Havza segment of North Anatolian Transform Fault Zone (NATFZ) is dominated by a well developed right lateral strike-slip fault system.
Conclusion & Impact:Morpho-tectonic features with dextrally offset stream channels (7 km) and ground ruptures of the 1943 Ladik-Ilgaz earthquake of M 7.2 strongly suggest that the first fault system is an active right lateral strike-slip fault zone
🔬Design:Research Article
📍Scope:Comprehensive Sample
⚙️Variables:Domain Parameters
Abstract
The Beşpınar-Havza segment of North Anatolian Transform Fault Zone (NATFZ) is dominated by a well developed right lateral strike-slip fault system. This system consists of well developed single fault and/or fault sets. These fault sets are: (1) Köprübaşı fault set, (2) Dereköy fault set, (3) Çeltek fault set and (4) Beyviran fault set. According to the interpretation of these faults, direction of the compressional strees is 150°. Morpho-tectonic features with dextrally offset stream channels (7 km) and ground ruptures of the 1943 Ladik-Ilgaz earthquake of M 7.2 strongly suggest that the first fault system is an active right lateral strike-slip fault zone
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Cite This Article
DİRİK, K. (1994). NEOTECTONIC CHARACTERISTICS OF BEŞPINAR-HAVZA SEGMENT OF NORTH ANATOLIAN TRANSFORM FAULT ZONE. Maden Tetkik ve Arama Dergisi, Cilt: 116 - Sayı: 116, 46–46. https://ajindex.com/articles/54283
Abdüsselamoğlu, M,Ş., 1950, Almacıkdağı ile Mudurnu ve Göynük civarının jeolojisi: ist. Üniv. Fen Fak. Monograf. 14, istanbul. Allen, C.R., 1969, Active faulting in Northern Turkey: Contribution No. 1577, Div. of Geol. Sci. Calif. Int. of Technology. 1982, Comparİsions between the North Anatolian Fault of Turkey and the San Andreas Fault of California: Işıkara. A.M. ve Vogel, A., eds., Multidisciplinary approach to Earthpuake Prediction da., Wiesbaden, Friedrich, Vieweg and Sohn, 67-85. Ambraseys. N.N., 1970, Some characteristic features of the North Anatolian Fault Zone: Tectonophysics, 9, 143-165.
Anderson, E.M., 1951, The dynamics of faulting: Edinburg, Oliver and Boyd, 206. Arpat, E. ve Şaroğlu, F., 1975, Türkiye'deki bazı önemli genç tektonik olaylar: TJK Bült., 18, 1,91 -101. Barka, AA, 1981, Seismo-tectonic aspacts of the North Anatolian fault zone: Ph. D. Thesis in University of Bristol, England, p. 335 (yayımlanmamış). 1984, Kuzey Anadolu Fay Zonundaki bazı NeojenKuvatemer havzalarının jeolojisi ve tektonik evrimi: Ketin Simpozyumu, TJK Bült., 209-227. ve Gülen, L., 1987, Age and total displacement of the North Anatolian fault zone and its significance for the betler understandng of tectonic history and preseni day dynamics of the Eastern Mediterranean region: (abstract), Melih Tokay Geology Symposium 87,57-58. ve Hancock, P.L, 1984, Neotectonic deformation pattems in the convex-northward arc of the North Anatolian fault zone: Dixon, J. E, and Robertson, A.H.F., eds. The Geological Evolution of the Eastern Mediterraneân da., Geological Sodety of London, Special Publication, 17, 285-296. Başkan ve Bulutçu, 1970, Havza (Samsun) kaplıcası hidrojeoloji etüdü raporu: MTA Rap., 4373 (yayımlanmamış), Ankara.
Bergougnan, H. ve Forquin, C., 1982, "Paleo-, Tardi- and Neotectonic mechanism of the present North Anatolian Fault Zone in the light of structural history of the Eurasian margin in the Pontic ranges: Işıkara, A.M. and Vogel, A., eds., Multjdsciplinary approach to Earthouake Prediction da, Wiesbaden, Friedrich, Vıeweg and Sohn, 23-40.
Bicar, Z. ve Serdar, S., 1981, Bafra-Vezirköprü-Havza-Kavak Samsun sınırlı sahanın jeolojisi ve petrol olanakları: TPAO Rap., 1519, (yayımlanmamış). Bidde, KT. ve Christie-Blick, N., 1985, Strike slip deformation and sedmentation: Soc. Econ. Paleon. and Miner., Spec. Publ., 37, Tulsa. Oklahoma, USA. Blumenthal, M., 1937, Kızılırmak ile Yeşilırmak arasındaki mıntıkada bulunan linyit, idrakarbür ve bitümlü şist yataklan