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Offshore/onshore correlation of the North-Anatolian fault deformations in the Western Sea of Marmara

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Abstract

Newly collected high-resolution seismic reflection and magnetic data collected offshore of the Ganos Fault (NW Turkey) in the western Sea of Marmara, along the submerged portion of the North-Anatolian Fault, highlight the presence of a complex fault pattern. Based on these data, we propose a new tectonic model for this key region, connecting the onshore fault pattern to the transtensional basins of the deepest Sea of Marmara. According to this new model, three main faults control the deformation pattern of this region, fault SF1, a tectonic element that shapes the Tekirdağ Basin, and fault SF2, which although not affecting the sea floor, is structurally related to SF1. Another fault we called SF3, connects the offshore to the Ganos fault onshore creating a transtensional pattern nearby the shelf. All such kinematic indicators witness an incipient activity, and a seismogenic potential that should be determined by a detailed mapping of both the surficial expression of fault at the seafloor, and the deformation pattern observed in the post-glacial sedimentary sequence. The active fault pattern detected nearby the coastal areas and their structural relationships with the Tekirdağ basin show that it could be interpreted as a negative flower structure, which accommodates strain partitioning. This observation is crucial to seismic hazard assessments in this region that has been the site of destructive earthquakes in the recent and remote past.

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Fig. 1

modified from Yaltırak 2002; Vardar et al. 2014; Vardar 2019), b Locations of the seismic and magnetic profiles collected for this study; superimposed on the multi-beam bathymetry data from Grall et al. (2018)

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References

  • Aksoy ME, Meghraoui M, Vallée M, Çakır Z (2010) Rupture characteristics of the AD 1912 Mürefte (Ganos) earthquake segment of the North Anatolian fault (western Turkey). Geology 38:991994

    Google Scholar 

  • Aksu AE, Calon TJ, Hiscott RN, Yasar D (2000) Anatomy of the North Anatolian fault zone in the Marmara Sea, western Turkey. GSA Today 10:3–7

    Google Scholar 

  • Alp H, Vardar D, Alpar B, Ustaömer T (2018) Seismic evidence for change of the tectonic regime in Messinian, Northern Marmara Sea. Turkey J Asian Earth Sci 151:40–53

    Google Scholar 

  • Altınok Y, Alpar B, Yaltırak C (2003) Şarköy-Mürefte 1912 earthquake’s tsunami extension of the associated faulting in the Marmara Sea. Turkey J Seismolog 7:329–346

    Google Scholar 

  • Altunel E, Meghraoui M, Akyüz HS, Dikbas A (2004) Characteristics of the 1912 co-seismic rupture along the North Anatolian fault zone (Turkey): implications for the expected Marmara earthquake. Terra Nova 16:198–204

    Google Scholar 

  • Amante C, Eakins BW (2009). ETOPO1 1 Arc-Minute global relief model: procedures, data sources and analysis. NOAA Technical Memorandum NESDIS, NGDC-24, pp 19

  • Ambraseys NN, Finkel CF (1987) The Saros–Marmara earthquake of 9 August 1912. Earthq Eng Struct D 15:189–211

    Google Scholar 

  • Ambraseys NN, Jackson JA (2000) Seismicity of Sea of Marmara (Turkey) since 1500. Geophys J Int 141:1–6

    Google Scholar 

  • Armijo R, Meyer B, Navarro S, King G, Barka A (2002) Asymmetric slip partitioning in the Sea of Marmara pull-apart: a clue to propagation processes of the North Anatolian fault. Terra Nova 14:80–86

    Google Scholar 

  • Armijo R, Pondard N, Meyer B, Ucarkus G, de Lepinay BM, Malavieille J, Dominguez S, Gustcher MA et al (2005) Submarine fault scarps in the Sea of Marmara pull-apart (North Anatolian Fault): Implications for seismic hazard in Istanbul. Geochem Geophys Geosys 6:1–29

    Google Scholar 

  • Ateş A, Bilim F, Büyüksaraç A, Bektas Ö (2008) A tectonic interpretation of the Marmara Sea, NW Turkey from geophysical data. Earth Planet Sp 60:169–177

    Google Scholar 

  • Barka AA, Kadinsky-Cade K (1988) Strike-slip fault geometry in Turkey and its influence on earthquake activity. Tectonics 7:663–684

    Google Scholar 

  • Briggs JC (1974) Machine contouring using minimum curvature. Geophysics 39:39–48

    Google Scholar 

  • Brothers D, Driscoll N, Kent G, Harding AJ, Babcock JM, Baskin RL (2009) Tectonic evolution of the Salton Sea inferred from seismic reflection data. Nature Geosci 2:581–584

    Google Scholar 

  • Demirbağ E, Rangin C, Le Pichon X, Şengör AC (2003) Investigation of the tectonics of the Main Marmara Fault by means of deep-towed seismic data. Tectonophysics 361:1–19

    Google Scholar 

  • Demirel S, Alpar B, Yaltırak C, Vardar D, Kurt H (2020) Northern segment of the North Anatolian Fault in the Gulf of Izmit inferred from marine magnetic anomalies. Mar Geophys Res 41:6. https://doi.org/10.1007/s11001-020-09399-6

    Article  Google Scholar 

  • Doo WB, Hsu SK, Armada L (2015) New magnetic anomaly map of the East Asia with some preliminary tectonic interpretations. Terr Atmos Ocean Sci 26:73–81

    Google Scholar 

  • Drab L, Hubert Ferrari A, Schmidt S, Martinez P (2012) The earthquake sedimentary record in the western part of the Sea of Marmara. Turkey Nat Hazards Earth Syst Sci 12:1235–1254

    Google Scholar 

  • Ergun M, Özel E (1995) Structural relationship between the Sea of Marmara Basin and North Anatolian Fault Zone. Terra Nova 7:278–288

    Google Scholar 

  • Gasperini L, Polonia A, Bortoluzzi G, Henry P, Lepichon X, Tyron M, Cagatay N, Geli L (2011a) How far did the surface rupture of the 1999 Izmit earthquake reach in Sea of Marmara? Tectonics. https://doi.org/10.1029/2010TC002726

    Article  Google Scholar 

  • Gasperini L, Polonia A, Çağatay N, Bortoluzzi G, Ferrante V (2011b) Geological slip rates along the North Anatolian Fault in the Marmara region. Tectonics. https://doi.org/10.1029/2011TC002906

    Article  Google Scholar 

  • Gasperini L, Lazar M, Mazzini A, Lupi M, Haddas A, Hensen C, Schmidt M, Caracausi A, Ligi M, Polonia A (2020) Neotectonics of the Sea of Galilee (northeast Israel): implication for geodynamics and seismicity along the Dead Sea Fault system. Sci Rep 10:11932

    Google Scholar 

  • Golynsky AV, Ivanov SV, Kazankov AJ, Jokat W, Masolov VN, von Frese RRB, The ADMAP Working Group (2013) New continental margin magnetic anomalies of East Antarctica. Tectonophysics 585:172–184

    Google Scholar 

  • Görür N, Çağatay MN, Sakınç M, Sümengen M, Şentürk K, Yaltırak C, Tchapalyga A (1997) Origin of the Sea of Marmara as deduced from Neogene to Quaternary paleogeographic evolution of its frame. Int Geol Rev 39:342–352

    Google Scholar 

  • Grall C, Dupre S, Guerin C, Normand A, Gaillot A, Fleury J, Henry P (2018) Processed AsterX AUV data from the Sea of Marmara: high-resolution bathymetry and seafloor backscatter images. SEANOE. https://doi.org/10.17882/55744

  • Guevara NO, Garcia A, Arnaiz M (2013) Magnetic anomalies in the Eastern Caribbean. Int J Earth Sci 102:591–604

    Google Scholar 

  • Gutzwiller K (1923). Die Milchverarbeitung in der Schweiz und der Handel mit Milcherzeugnissen. Schweiz. Milchwirtsch. Sekretariat. Meer: Thesis. Basel University, p 25

  • Gurbuz C, Aktar M, Eyidogan H, Cisternas A, Haessler H, Barka A, Ergin M, Turkelli N et al (2000) The seismotectonics of the Marmara region (Turkey): results from a microseismic experiment. Tectonophysics 316:1–17

    Google Scholar 

  • Imren C, Le Pichon X, Rangin C, Demirbağ E, Ecevitoğlu B, Görür N (2001) The North Anatolian Fault within the Sea of Marmara: a new interpretation based on multi-channel seismic and multi-beam bathymetry data. Earth Planet Sci Lett 186:143–158

    Google Scholar 

  • Janssen C, Bohnhoff M, Vapnik Y, Görgün E, Bulut F, Plessen B, Pohl D, Aktar M et al (2009) Tectonic evolution of the Ganos segment of the North Anatolian Fault (NW Turkey). J Struct Geol 31:11–28. https://doi.org/10.1016/j.jsg.2008.09.010(ISSN0191-8141)

    Article  Google Scholar 

  • Judd AG, Hovland M (1992) The evidence of shallow gas in marine sediments. Cont Shelf Res 12(10):1081–1095. https://doi.org/10.1016/0278-4343(92)90070-Z

    Article  Google Scholar 

  • Karabulut H, Roumelioti Z, Benetatos C, Ahu Komec M, Özalaybey S, Aktar M, Kiratzi A (2006) A source study of the 6 July 2003 (Mw 5.7) earthquake sequence in the Gulf of Saros (northern Aegean Sea): seismological evidence for the western continuation of the Ganos fault. Tectonophysics 412:195–216. https://doi.org/10.1016/j.tecto.2005.09.009

    Article  Google Scholar 

  • Kende J, Henry P, Bayrakçı G, Özeren MS, Grall C (2017) Moho depth and crustal thinning in the Marmara Sea region from gravity data inversion. J Geophys Res Solid Earth 122:1381–1401. https://doi.org/10.1002/2015JB012735

    Article  Google Scholar 

  • Kurt H, Demirbaǧ E, Kuşçu İ (2000) Active submarine tectonism and formation of the Gulf of Saros, Northeast Aegean Sea, inferred from multi-channel seismic reflection data. Mar Geol 165:13–26

    Google Scholar 

  • Laigle M, Becel A, de Voogd B, Hirn A, Taymaz T, Ozalaybey S, The Members of the SEISMARMARA Leg1 (2008) A first deep seismic survey in the Sea of Marmara: whole crust and deep basins. Earth Planet Sci Lett 270:168–179

    Google Scholar 

  • Le Pichon X, Chamot-Rooke N, Rangin C, Şengör AMC (2003) The North Anatolian fault in the Sea of Marmara. J Geophys Res. https://doi.org/10.1029/2002JB001862

    Article  Google Scholar 

  • Li CF, Cheng B, Zhou ZY (2009) Deep crustal structures of eastern China and adjacent seas revealed by magnetic data. Sci China Ser D 52:984–993

    Google Scholar 

  • Meghraoui M, Aksoy ME, Akyüz HS, Ferry M, Dikbaş A, Altunel E (2012) Paleoseismology of the North Anatolian fault at Güzelköy (Ganos segment, Turkey): size and recurrence time of earthquake ruptures west of the Sea of Marmara. Geochem Geophys Geosyst 13(4):Q04005. https://doi.org/10.1029/2011GC003960

    Article  Google Scholar 

  • Meyer B, Saltus R, Chulliat A (2017). EMAG2: Earth Magnetic Anomaly Grid (2-arc-minute resolution) Version 3. National Centers for Environmental Information. NOAA. Model. DOI: https://doi.org/10.7289/V5H70CVX [10.04.2020]

  • Okay A, Demirbağ E, Kurt H, Okay N, Kuşçu İ (1999) An active, deep marine strike-slip basin along the North Anatolian fault in Turkey. Tectonics 18:129–147

    Google Scholar 

  • Okay AI, Kazlilar-Ozcan A, İmren C, Boztepe-Güney A, Demirbağ E, Kuşçu İ (2000) Active faults and evolving strike-slip basins in the Marmara Sea, Northwest Turkey from a multichannel seismic reflection study. Tectonophysics 321:189–218

    Google Scholar 

  • Okay AI, Tüysüz O, Kaya Ş (2004) From transpression to transtension: changes in morphology and structure around a bend on the North Anatolian Fault in the Marmara region. Tectonophysics 391:259–282

    Google Scholar 

  • Öztürk YK, Özal NM, Özbakir AD (2015) States of local stresses in the Sea of Marmara through the analysis of large numbers of small earthquakes. Tectonophysics 665:37–57. https://doi.org/10.1016/j.tecto.2015.09.027(ISSN0040-1951)

    Article  Google Scholar 

  • Parke JR, White RS, McKenzie D, Minshull TA, Bull JM, Kuscu I, Gorur N, Sengor C (2002) Interaction between faulting and sedimentation in the Sea of Marmara, Western Turkey. J Geophys Res Solid Earth 107:EPM 2-1-EPM 2-20

    Google Scholar 

  • Parsons T (2004) Recalculated probability of M 7 earthquakes beneath the Sea of Marmara Turkey. J Geophys Res 109:B05304

    Google Scholar 

  • Polonia A, Gasperini L, Amorosi A, Bonatti E, Çağatay N, Capotondi L, Cormier M-H, Görür N, McHugh C, Seeber L (2004) Holocene Slip rate of the North Anatolian Fault beneath the Sea of Marmara. EPSL 427:411–426

    Google Scholar 

  • Rangin E, Demirbağ C, İmren A, Crusson E, Normand E, Le Drezen A, Le Bot (2001) Marine Atlas of the Sea of Marmara (Turkey) IFREMER—Brest Technology Center

  • Rockwell T, Barka A, Dawson T, Akyuz S, Thorup K (2001) Paleoseismology of the GazikoySaros segment of the North Anatolia fault, northwestern Turkey: comparison of the historical and paleoseismic records, implications of regional seismic hazard, and models of earthquake recurrence. J Seismol 5:433–448

    Google Scholar 

  • Seeber L, Emre O, Cormier MH, Sorlien CC, McHugh CMG, Polonia A, Ozer N, Cagatay N (2004) Uplift and subsidence from oblique slip: the Ganos–Marmara bend of the North Anatolian Transform, Western Turkey. Tectonophysics 391:239–258

    Google Scholar 

  • Sengör AMC (1979) The North Anatolian transform fault: its age, offset and tectonic significance. J Geol Soc London 136(3):269–282

    Google Scholar 

  • Şengör AMC, Grall C, İmren C, Le Pichon X, Görür N, Henry P, Karabulut H, Siyako S (2014) The geometry of the North Anatolian transform fault in the Sea of Marmara and its temporal evolution: implications for the development of intracontinental transform faults. Can J Earth Sci 51:222–242

    Google Scholar 

  • Talwani M (1965) Computation with the help of a digital computer of magnetic anomalies caused by bodies of arbitrary shape. Geophysics 30:797–817. https://doi.org/10.1190/1.1439654

    Article  Google Scholar 

  • Teknik V, Thybo H, Artemiev IM (2020). Magmatic arcs, ophiolite belts and sedimentary basins in Anatolia interpreted from magnetic data. EGU, 4–8 May 2020, Vienna, Austria

  • Thébault E, Finlay CC, Alken P, Beggan CD, Canet E, Chulliat A, Langlais B, Lesur V et al (2015) Evaluation of candidate geomagnetic feld models for IGRF-12. Earth Planets Space. https://doi.org/10.1186/s40623-015-0228-9

    Article  Google Scholar 

  • Tüysüz O, Barka A, Yiğitbaş E (1998) Geology of the Saros graben and its implications for the evolution of the North Anatolian fault in the Ganos-Saros region, northwestern Turkey. Tectonophysics 293:105–126

    Google Scholar 

  • Utkucu M, Kanbur Z, Alptekin Ö, Sünbül F (2009) Seismic behaviour of the North Anatolian Fault beneath the Sea of Marmara (NW Turkey): implications for earthquake recurrence times and future seismic hazard. Nat Hazard 50:45–71

    Google Scholar 

  • Ustaomer T, Gokasan E, Tur H, Gorum T, Batuk F, Kalafat D, Alp H, Ecevitoglu B, Birkan H (2008) Faulting, masswasting and deposition in an active dextral shear zone, the Gulf of Saros and the NE Aegean Sea, NW Turkey. Geo-Mar Lett 28:171–193

    Google Scholar 

  • Vardar D, Öztürk K, Yaltırak C, Alpar B, Tur H (2014) Late Pleistocene-Holocene evolution of the southern Marmara shelf and sub-basins: middle strand of the North Anatolian fault, southern Marmara Sea. Turkey Mar Geohys Res 35:69–85

    Google Scholar 

  • Vardar D (2019) Evidence for active faulting in the eastern part of the Gulf of Saros, northern Aegean, from high-resolution seismic data. J Earth Syst Sci 128:52. https://doi.org/10.1007/s12040-019-1084-y

    Article  Google Scholar 

  • Wong HK, Lüdman T, Uluğ A, Görür N (1995) The Sea of Marmara; a plate boundary sea in an escape tectonic regime. Tectonophysics 244:231–250

    Google Scholar 

  • Yaltırak C (1996) Tectonic history of the Ganos fault system. Bull Turkish As Petrol Geol 8:137–156

    Google Scholar 

  • Yaltırak C, Alpar B, Yüce H (1998) Tectonic elements controlling the evolution of the Gulf of Saros (northeastern Aegean Sea, Turkey). Tectonophysics 300:227–248

    Google Scholar 

  • Yaltırak C, Alpar B, Sakınç M, Yüce H (2000) Origin of the Strait of Çanakkale (Dardanelles): regional tectonics and the Mediterranean—Marmara incursion. Mar Geol 164:139–156

    Google Scholar 

  • Yaltırak C (2002) Tectonic evolution of the Marmara Sea and its surroundings. Mar Geol 190:493529

    Google Scholar 

  • Yaltırak C, Alpar B (2002) Kinematics and evolution of the Northern branch of the North Anatolian Fault (Ganos Fault) between the Sea of Marmara and the Gulf of Saros. Mar Geol 190:351–366

    Google Scholar 

  • Yaltırak C, Sakınç M, Aksu AE, Hiscott RN, Galleb B, Ülgen UB (2002) Late Pleistocene uplift history along the Southwestern Marmara Sea determined from raised coastal deposits and global sea-level variations. Mar Geol 190:283–305

    Google Scholar 

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Acknowledgements

The authors gratefully acknowledge the financial support of the Scientific and Technological Research Council of Turkey-TUBITAK (Project 118Y079). We gratefully acknowledge A.C. Yalçıner who shed us light in every conversation we made. We thank to Luca Gasperini and anonymous reviewer for their comments and suggestions. The Kingdom Suite® seismic package was kindly made available by IHS Kingdom Educational Grant Program. Some CHIRP profiles were processed by using ECHOS seismic data processing software.

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Correspondence to Denizhan Vardar.

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Vardar, D., Alp, H., Demirel, S. et al. Offshore/onshore correlation of the North-Anatolian fault deformations in the Western Sea of Marmara. Nat Hazards 107, 1905–1923 (2021). https://doi.org/10.1007/s11069-021-04664-2

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