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Source Characteristics of the January 8, 2013 (M w = 5.7) and May 24, 2014 (M w = 6.8) North Aegean Earthquakes Sequence

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Abstract

The Aegean Sea, is one of the most seismically active areas of the Eastern Mediterranean region (Fig. 1). Generally, North Aegean Sea region has been tectonically developed after the collision of Arabian plate with the Eurasian in the Late Miocene time and the subsequent westward escape of the Anatolian Plate relative to the Eurasian Plate, during the Early Pliocene.

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References

  • Aksoy ME, Meghraoui M, Vallée M, Çakır Z (2010) Rupture characteristics of the A.D. 1912 Mürefte (Ganos) earthquake segment of the North Anatolian fault (western Turkey). Geology 1(38):991–994

    Article  Google Scholar 

  • Allen CR (1969) Active faulting in northern Turkey, Contr. No. 1577. Div Geol Sci Calf Inst Tech 32

    Google Scholar 

  • Barka AA (1992) The North Anatolian Fault zone. Annales Tectonicae 6:164–195

    Google Scholar 

  • Barka A, Gülen L (1988) New constrains on age and total offset on the North Anatolian Fault Zone: implications for tectonics of the Eastern Mediterranean Region. METU J Pure Appl Sci 21:39–63

    Google Scholar 

  • Barka AA, Toksöz MN, Gülen L, Kadinsky-Cade K (1987) Kuzey Anadolu Fayının Doğu Kesiminin Segmentasyonu, Sismisitesi ve Deprem Potansiyeli, Yerbilimleri C14:337–352

    Google Scholar 

  • Chatzipetros A, Kiratzi A, Sboras S, Zouros N, Pavlides S (2013) Active faulting in the north-eastern Aegean Sea Islands. Tectonophysics 597–598:106–122

    Article  Google Scholar 

  • Dewey JF (1976) Seismicity of Northern Anatolia. Bull Seis Soc Am 3:843–868

    Google Scholar 

  • Dewey JF, Şengör AMC (1979) Aegean and surrounding regions: Complex multiplate and continuum tectonics in a convergent zone. Geol Soc Am Bull 90:84–92. https://doi.org/10.1130/0016-7606

    Article  Google Scholar 

  • Drakopoulos JC, Ekonomides AC (1972) Aftershocks of February 19, 1968 earthquake in Northern Aegean Sea and Related Problems. Pure Appl Geophys 95(1):100–115

    Google Scholar 

  • Dreger D (2002) Manual of the time-domain moment tensor inverse code (TDMT_INVC), Release 1.1. Berkeley Seismology Laboratory, p 18

    Google Scholar 

  • Ergintav S, Doğan U, Gerstenecker C, Çakmak R, Belgen A, Demirel H, Aydın C, Reilinger R (2007) A snapshot (2003–2005) of the 3D postseismic deformation for the 1999, Mw = 7.4 İzmit Earthquake in the Marmara Region, Turkey, by first results of joint gravity and GPS monitoring. J Geodyn 44(1):1–18

    Article  Google Scholar 

  • Eyidoğan H, Güçlü U, Utku Z, Değirmenci E (1991) Türkiye Büyük Depremleri Makro -Sismik Rehberi (1900–1988). İTÜ Maden Fak. Jeofizik Müh. Böl, İstanbul

    Google Scholar 

  • Ganas A, Roumelioti Z, Karastathis V, Chousianitis K, Moshou A, Mouzakiotis E (2014) The Lemnos January 2013 (Mw = 5.7) earthquake: fault slip, aftershock properties and static stress transfer modeling in the north Aegean Sea. J Seismol 2014(18):433–455

    Article  Google Scholar 

  • Genç CŞ, Altunkaynak Ş, Karacık Z, Yazman M, Yılmaz Y (2001) The Çubukludağ graben, south of İzmir: its tectonic significance in the Neogene geological evolution of the western Anatolia. Geodin Acta 14(1–3):45–55

    Google Scholar 

  • Gephart JW (1990) FMSI: A FORTRAN program for inverting fault/slickenside and earthquake focal mechanism data to obtain the regional stress tensor. Com Geosci 16:953–989

    Article  Google Scholar 

  • Goldsworthy M, Jackson J, Haines J (2002) The continuity of active fault systems in Greece. Geophys J Int 148:596–618

    Article  Google Scholar 

  • Görgün E, Görgün B (2015) Seismicity of the 24 May 2014 Mw 7.0 Aegean Sea earthquake sequence along the North Aegean Trough. J Asian Earth Sci 111:459–469

    Article  Google Scholar 

  • Jackson J, McKenzie DP (1984) Active tectonics of the Alpine-Himalayan Belt between Western Turkey and Pakistan. Geophys J R Astr Soc 77:185–246

    Article  Google Scholar 

  • Kalafat D, Gürbüz C, Üçer SB (1987) Batı Türkiye’de Kabuk ve Üst Manto Yapısının Araştırılması. Deprem Araştırma Bülteni, Sayı 59:43–64 (in Turkish)

    Google Scholar 

  • Kalafat D, Kekovalı K, Güneş Y, Yılmazer M, Kara M, Deniz P, Berberoğlu M (2009) Türkiye ve Çevresi Faylanma-Kaynak Parametreleri (MT) Kataloğu (1938–2008): A catalogue of source parameters of moderate and strong earthquakes for Turkey and its surrounding area (1938–2008). Boğaziçi University Publication,Bebek-İstanbul, no 1026, 43 pp

    Google Scholar 

  • Kalafat D, Güneş Y, Kekovalı K, Kara M, Deniz P, Yılmazer M (2011) Bütünleştirilmiş Homojen Deprem Kataloğu (1900–2010; M ≥4.0)—a revised and extended earthquake catalogue for Turkey since 1900 (1900–2010; M ≥4.0). Boğaziçi University Library Cataloging-in Publication Data, İstanbul, 640 pp

    Google Scholar 

  • Karakostas VG, Papadimitriou EE, Karakaisis GF, Papazachos CB, Scordilis EM, Vargemezis G, Aidona E (2003) The 2001 Skyros, Northern Aegean, Greece, earthquake sequence: off-fault aftershocks, tectonic implications, and seismicity triggering. Geophys Res Lett 30(1):1012. https://doi.org/10.1029/2002gl015814

    Article  Google Scholar 

  • Kikuchi M, Kanamori H (2003) Note on teleseismic body-wave inversion program. http://www.eri.u-tokyo.ac.jp/ETAL/KIKUCHI

  • Kiratzi AA (2002) Stress tensor inversions along the westernmost North Anatolian Fault Zone and its continuation into the North Aegean Sea. Geophys J Int 151:360–376

    Article  Google Scholar 

  • Kiratzi AA, Svigkas N (2013) A study of the 8 January 2013 Mw5.8 earthquake sequence (Lemnos Island, East Aegean Sea). Tectonophysics 608:452–460. http://dx.doi.org/10.1016/j.tecto.2013.09.002

    Article  Google Scholar 

  • Klein FW (2002) User’s Guide to HYPOINVERSE–2000, a Fortran program to solve for earthquake locations and magnitudes, USGS Open-File Report 02-171

    Google Scholar 

  • Koukouvelas I, Aydin A (2002) Fault structure and related basins of the North Aegean Sea and its surroundings. Tectonics 21(5)

    Article  Google Scholar 

  • Kreemer C, Chamot-Rooke N, Le Pichon X (2004) Constraints on the evolution and vertical coherency of deformation in the Northern Aegean from a comparison of geodetic, geologic and seismologic data. Earth Planet Sci Lett 225(3–4):346. https://doi.org/10.1016/j.epsl.2004.06.018

    Article  Google Scholar 

  • Kürçer A, Yalçın H, Gülen L, Kalafat D (2015) 8 January 2013 Mw = 5.7 North Aegean Sea Earthquake and its seismotectonic significance. Geodin Acta. https://doi.org/10.1080/09853111.2014.957503

    Article  Google Scholar 

  • Le Pichon X, Lybéris N, Alvarez F (1987) Discussion on the subsidence of the North Aegean Trough: an alternative view. J Geol Soc 144(2):349–351. https://doi.org/10.1144/gsjgs.144.2.0349

  • Lee WHK, Lahr JC (1975) HYPO71: a computer program for determining hypocenter, magnitude and first motion pattern of local earthquakes. USGS Open File Rep 75–311:1–116

    Google Scholar 

  • McClusky S, Balassanian S, Barka A, Demir C, Ergintav S, Georgiev I, Gurkan O, Hamburger M, Hurst K, Kahle H, Kastens K, Kekelidze G, King R, Kotzev V, Lenk O, Mahmoud S, Mishin A, Nadariya M, Ouzounis A, Paradisis D, Peter Y, Prilepin M, Reilinger R, Sanli I, Seeger H, Tealeb A, Toksöz MN, Veis G (2000) Global Positioning System constraints on plate kinematics and dynamics in the eastern Mediterranean and Caucasus. J Geophys Res 105(B3):5695–5719

    Article  Google Scholar 

  • McKenzie D (1972) Active tectonics of the Mediterranean region. Geophys J R Astr Soc 30(2):109–185. https://doi.org/10.1111/j.1365-246x.1972.tb02351.x

    Article  Google Scholar 

  • McKenzie D (1978) Active tectonics of the Alpine-Himalayan belt, the Aegean Sea and surrounding regions. Geophys J Roy Astron Soc 55:217–254

    Article  Google Scholar 

  • McKenzie D, Jackson J (1983) The relationship between strain rates, crustal thickening, paleomagnetism, finite strain and fault movements within a deforming zone. Earth Planet Sci Lett 65:182–202

    Article  Google Scholar 

  • Papadimitriou EE, Sykes LR (2001) Evolution of the stress field in the northern Aegean Sea (Greece). Geophys J Int 146(3):747–759

    Article  Google Scholar 

  • Papazachos CB (1999) Seismological and GPS evidence for the Aegean–Anatolia interaction. Geophys Res Lett 26(17):2653–2656. https://doi.org/10.1029/1999gl.900411

    Article  Google Scholar 

  • Papazachos BC, Papadimitriou EE, Kiratzi AA, Papazachos CB, Louvari EK (1998) Fault plane solutions in the Aegean Sea and the surrounding area and their tectonic implication. Boll Geof Teor Appl 39(3):199–218

    Google Scholar 

  • Papazachos BC, Karakaisis GF, Papazachos CB, Scordilis EM (2000) Earthquake triggering in the North and East Aegean Plate Boundaries due to the Anatolia Westward Motion. Geophys Res Lett 27. https://doi.org/10.1029/2000GL011425. issn: 0094–8276.

    Article  Google Scholar 

  • Pınar A, Kuge K, Honkura Y (2003) Moment tensor inversion of recent small to moderate sized earthquakes: implications for seismic hazard and active tectonics beneath the Sea of Marmara. Geophys J Int 153:133–145

    Article  Google Scholar 

  • Reilinger R, McClusky S, Oral B, King R, Toksoz M, Barka A, Kinik I, Lenk O, Sanli I (1997) GPS measurements of present-day crustal movements in the Arabia Africa-Eurasia Plate collision zone. J Geophys Res 102(9983–9999):1997

    Google Scholar 

  • Saikia C (1994) Modified frequency-wave number algorithm for regional seismo-grams using Filon’s quadrature; modelling of Lg waves in eastern North America. Geophys J Int 118:142–158

    Article  Google Scholar 

  • Saltogianni V, Gianniou M, Taymaz T, Yolsal-Çevikbilen S, Stiros S (2015) Fault slip source models for the 2014 M w  6.9 Samothraki-Gökçeada earthquake (North Aegean Trough) combining geodetic and seismological observations. J Geophys Res Solid Earth 120(12):8610–8622

    Google Scholar 

  • Şaroğlu F, Emre Ö, Herece E (1992) MTA Genel Müdürlüğü web site 1.500 000 scale geological map

    Google Scholar 

  • Şengör AMC, Görür N, Şaroğlu F (1985) Strike-slip deformation, basin formation and sedimentation. Soc Econ Paleontol Mineral Spc Publ 37:227–264

    Google Scholar 

  • Taymaz T, Jackson J, McKenzie D (1991) Active tectonics of the north and central Aegean Sea. Geophys J Int 106:433–490

    Article  Google Scholar 

  • Vannucci G, Gasperini P (2003) The earthquake mechanisms of the Mediterranean Area (EMMA). http://www.emsc-csem.org/Earthquake/emma.php

  • Wells DL, Coppersmith KJ (1994) New empirical relationships among magnitude, rupture length, rupture width, rupture area, and surface displacement. Bull Seismol Soc Am 84(4):974–1002

    Google Scholar 

  • Wiemer S, Katsumata K (1999) Spatial variability of seismicity parameters in aftershock zones. J Geophys Res 104:13135–13151

    Article  Google Scholar 

  • Wiemer S, Wyss M (2002) Spatial and temporal variability of the b-value in seismogenic volumes: an overview. Adv Geophys 45:259–302

    Article  Google Scholar 

  • Yaltırak C, İşler EB, Aksu AE, Hiscott RN (2012) Evolution of the Bababurnu Basin and shelf of the Biga Peninsula: western extension of the middle strand of the North Anatolian Fault Zone, Northeast Aegean Sea, Turkey. J Asian Earth Sci 57(2012):103–119

    Article  Google Scholar 

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Acknowledgements

The first author was supported by the Department of Science Fellowship and Grant programs (2014-2219) of TUBITAK (The Scientific and Technological Research Council of Turkey). Also this study was supported by Bogazici University Research Projects Commission under SRP/BAP project No. 6040.

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Correspondence to Doğan Kalafat .

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Kalafat, D., Kekovalı, K., Pınar, A. (2018). Source Characteristics of the January 8, 2013 (M w = 5.7) and May 24, 2014 (M w = 6.8) North Aegean Earthquakes Sequence. In: D'Amico, S. (eds) Moment Tensor Solutions. Springer Natural Hazards. Springer, Cham. https://doi.org/10.1007/978-3-319-77359-9_16

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