Skip to main content
Log in

The Lemnos 8 January 2013 (M w = 5.7) earthquake: fault slip, aftershock properties and static stress transfer modeling in the north Aegean Sea

  • Original Article
  • Published:
Journal of Seismology Aims and scope Submit manuscript

An Erratum to this article was published on 10 September 2014

Abstract

We investigate mainshock slip distribution and aftershock activity of the 8 January 2013 M w = 5.7 Lemnos earthquake, north Aegean Sea. We analyse the seismic waveforms to better understand the spatio-temporal characteristics of earthquake rupture within the seismogenic layer of the crust. Peak slip values range from 50 to 64 cm and mean slip values range from 10 to 12 cm. The slip patches of the event extend over an area of dimensions 16 × 16 km2. We also relocate aftershock catalog locations to image seismic fault dimensions and test earthquake transfer models. The relocated events allowed us to identify the active faults in this area of the north Aegean Sea by locating two, NE–SW linear patterns of aftershocks. The aftershock distribution of the mainshock event clearly reveals a NE–SW striking fault about 40 km offshore Lemnos Island that extends from 2 km up to a depth of 14 km. After the mainshock most of the seismic activity migrated to the east and to the north of the hypocenter due to (a) rupture directivity towards the NE and (b) Coulomb stress transfer. A stress inversion analysis based on 14 focal mechanisms of aftershocks showed that the maximum horizontal stress is compressional at N84°E. The static stress transfer analysis for all post-1943 major events in the North Aegean shows no evidence for triggering of the 2013 event. We suggest that the 2013 event occurred due to tectonic loading of the North Aegean crust.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9
Fig. 10

Similar content being viewed by others

References

  • Altinok Y, Alpar B, Yaltirak C, Pinar A, Ӧzer N (2012) The earthquakes and related tsunamis of October 6, 1944 and March 7, 1867; NE Aegean Sea. Nat Hazards 60(1):3–25. doi:10.1007/s11069-011-9949-7

    Article  Google Scholar 

  • Benetatos C, Roumelioti Z, Kiratzi A, Melis N (2002) Source parameters of the M 6.5 Skyros Island (North Aegean Sea) earthquake of July 26, 2001. Ann Geophys 45(3–4):513–526

    Google Scholar 

  • Brooks M, Ferentinos G (1980) Structure and evolution of the Sporades basin of the north Aegean trough, northern Aegean Sea. Tectonophysics 68(1–2):15–30. doi:10.1016/0040-1951(80)90006-2

    Article  Google Scholar 

  • Caputo R, Chatzipetros A, Pavlides S et al (2012) The Greek database of Seismogenic sources (GreDaSS): state-of-the-art for northern Greece. Ann Geophys 55(5):859–894. doi:10.4401/ag-5168

    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, ISSN 0040-1951, doi:10.1016/j.tecto.2012.11.026

  • Dreger D (1994) Empirical Green’s function study of the January 17, 1994 Northridge, California earthquake. Geophys Res Lett 21:2633–2636

    Article  Google Scholar 

  • Dreger D (2002) Time-domain moment tensor INVerse code (TDMT_INVC) Version 1.1, Berkeley Seismological Laboratory, 18

  • Dreger DS (2003) TDMT_INV: time domain seismic moment tensor INVersion, international handbook of earthquake and engineering seismology. In: Lee WHK, Kanamori H, Jennings PC, Kisslinger C (eds), vol. B. Academic Press, London, p 1627

  • Dreger D, Helmberger D (1993) Determination of source parameters at regional distances with single station or sparse network data. J Geophys Res 98:8107–8125

    Article  Google Scholar 

  • Ganas A, Drakatos G, Pavlides SB, Stavrakakis GN, Ziazia M, Sokos E, Karastathis VK (2005) The 2001 Mw = 6.4 Skyros earthquake, conjugate strike–slip faulting and spatial variation in stress within the central Aegean Sea. J Geodyn 39:61–77

    Article  Google Scholar 

  • Ganas A, Roumelioti Z, Chousianitis K (2012) Static stress transfer from the May 20, 2012, M 6.1 Emilia-Romagna (northern Italy) earthquake using a co-seismic slip distribution model. Ann Geophys, Special Issue entitled “The Emilia seismic sequence of May–June, 2012: preliminary data and results”. 55(4) doi:10.4401/ag-6176

  • Gomberg J, Reasenberg PA, Bodin P, Harris RA (2001) Earthquake triggering by seismic waves following the Landers and Hector mine earthquakes. Nature 411:462–466

    Article  Google Scholar 

  • Harris RA, Simpson RW (1998) Suppression of large earthquakes by stress shadows: a comparison of Coulomb and rate and state failure. J Geophys Res 103:439–451

    Article  Google Scholar 

  • Hartzell SH (1978) Earthquake aftershocks as Green’s functions. Geophys Res Lett 5(1):1–4

    Article  Google Scholar 

  • Hatzfeld D, Ziazia M, Kementzetzidou D, Hatzidimitriou P, Panagiotopoulos D, Makropoulos K, Papadimitriou P, Deschamps A (1999) Microseismicity and focal mechanisms at the western termination of the North Anatolian Fault and their implications for continental tectonics. Geophys J Int 137:891–908

    Article  Google Scholar 

  • Kalogeras, I., Melis, N., Evangelides, C., (2013) The earthquake of January 8, 2013 at SE of Limnos Island, Northern Aegean, Greece. NOA online report at http://www.gein.noa.gr/Documents/pdf/Report_EN_PDF.pdf (last accessed 23 December 2013)

  • Karabulut H, Roumelioti Z, Benetatos C, Mutlu A, Ozalaybey 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

    Article  Google Scholar 

  • Karagianni EE, Papazachos CB, Panagiotopoulos DG, Suhaldoc P, Vuan A, Panza GF (2005) Shear velocity structure in the Aegean area obtained by inversion of Rayleigh waves. Geophys J Int 160:127–143

    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

    Article  Google Scholar 

  • Kiratzi AA, Wagner GS, Langston CA (1991) Source parameters of some large earthquakes in northern Aegean determined by body waveform inversion. Pure Appl Geophys 135(4):515–527. doi:10.1007/bf01772403

    Article  Google Scholar 

  • Konstantinou KI, Melis NS, Boukouras K (2010) Routine regional moment tensor inversion for earthquakes in the Greek region; the National Observatory of Athens (NOA) database (2001–2006). Seismol Res Lett 81(5):750–760

    Article  Google Scholar 

  • Koukouvelas IK, Aydin A (2002) Fault structure and related basins of the North Aegean Sea and its surroundings. Tectonics 21(5), doi:10.1029/2001TC901037

  • 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):329–346. doi:10.1016/j.epsl.2004.06.018

    Article  Google Scholar 

  • Le Meur H (1994) Tomographie tridimensionnelle a partir des temps des premieres arrivees des ondes P et S, application a la region de Patras (Grece). PhD thesis, Paris VII, France (in French)

  • Le Meur H, Virieux J, Podvin P (1997) Seismic tomography of the gulf of Corinth: a comparison of methods. Ann Geofis 40(6):1–24

    Google Scholar 

  • Lin J, Stein R (2004) Stress triggering in thrust and subduction earthquakes, and stress interaction between the southern San Andreas and nearby thrust and strike–slip faults. J Geophys Res 109, B02303. doi:10.1029/2003JB002607

    Google Scholar 

  • Lomax A, Virieux J, Volant P, Berge C (2000) Probabilistic earthquake location in 3D and layered models: introduction of a Metropolis–Gibbs method and comparison with linear locations. In: Thurber CH, Rabinowitz N (eds) Advances in seismic event location. Kluwer, Amsterdam, pp 101–134

    Chapter  Google Scholar 

  • Makropoulos K, Kaviris G, Kouskouna V (2012) An updated and extended earthquake catalogue for Greece and adjacent areas since 1900. Nat Hazards Earth Syst Sci 12:1425–1430

    Article  Google Scholar 

  • Michael AJ (1991) Spatial variations in stress within the 1987 Whittier narrows, California, aftershock sequence — new techniques and results. J Geophys Res 96(B4):6303–6319. doi:10.1029/91JB00195

    Article  Google Scholar 

  • Mori J, Hartzell S (1990) Source inversion of the 1988 Upland earthquake: determination of a fault plane for a small event. Bull Seismol Soc Am 80:278–295

    Google Scholar 

  • Müller MD, Geiger A, Kahle H, Veis G, Billiris H, Paradissis D, Felekis S (2013) Velocity and deformation fields in the north Aegean domain, Greece, and implications for fault kinematics, derived from GPS data 1993–2009. Tectonophysics 597–598:34–49

    Article  Google Scholar 

  • Nalbant SS, Hubert A, King GCP (1998) Stress coupling between earthquakes in northwest Turkey and the north Aegean Sea. J Geophys Res 103(B10):24469–24486. doi:10.1029/98JB01491

    Article  Google Scholar 

  • Novotný O, Zahradník J, Tselentis G-A (2001) North-Western Turkey earthquakes and the crustal structure inferred from surface waves observed in Western Greece. Bull Seismol Soc Am 91:875–879

    Article  Google Scholar 

  • Okada Y (1992) Internal deformation due to shear and tensile faults in a half-space. Bull Seismol Soc Am 82:1018–1040

    Google Scholar 

  • Panagiotopoulos DG, Hatzidimitriou PM, Karakaisis GF, Papadimitriou EE, Papazachos BC (1985) Travel time residuals in southeastern Europe. Pure Appl Geophys 123:221–231

    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. doi:10.1046/j.0956-540x.2001.01486.x

    Article  Google Scholar 

  • Papadopoulos G, Ganas A, Plessa A (2002) The Skyros earthquake (Mw6.5) of 26 July 2001 and precursory seismicity patterns in the North Aegean Sea. Bull Seismol Soc Am 92(30):1141–1145

    Article  Google Scholar 

  • Pasyanos M, Dreger D, Romanowicz B (1996) Towards real-time determination of regional moment tensors. Bull Seismol Soc Am 86:1255–1269

    Google Scholar 

  • Pavlides SB, Tranos MD (1991) Structural characteristics of 2 strong earthquakes in the north-Aegean — Ierissos (1932) and Agios-Efstratios (1968). J Struct Geol 13(2):205–214. doi:10.1016/0191-8141(91)90067-s

    Article  Google Scholar 

  • Podvin P, Lecomte I (1991) Finite difference computation of traveltimes in very contrasted velocity models: a massively parallel approach and its associated tools. Geophys J Int 105:271–284

    Article  Google Scholar 

  • Roumelioti Z, Dreger D, Kiratzi A, Theodoulidis N (2003) Slip distribution of the September 7, 1999 Athens earthquake inferred from an empirical Green’s function study. Bull Seismol Soc Am 93(2):775–782

    Article  Google Scholar 

  • Roumelioti Z, Benetatos C, Kiratzi A (2011) Time Domain Moment Tensors of earthquakes in the broader Aegean Sea for the years 2006–2007: the database of the Aristotle University of Thessaloniki. J Geodyn 51:179–189

    Article  Google Scholar 

  • Saikia CK (1994) Modified frequency–wavenumber algorithm for regional seismograms using Filon’s quadrature; modeling of Lg waves in eastern North America. Geophys J Int 118:142–158

    Article  Google Scholar 

  • Tarantola A (1987) Inverse problem theory: methods f8or data fitting and model parameter estimation. Elsevier, Amsterdam, 613p

    Google Scholar 

  • Tarantola A, Valette B (1982) Inverse problems = quest for information. J Geophys 50:159–170

    Google Scholar 

  • Taymaz T, Jackson J, Mckenzie D (1991) Active tectonics of the north and central Aegean Sea. Geophys J Int 106(2):433–490. doi:10.1111/j.1365-246X.1991. tb03906.x

    Article  Google Scholar 

  • Toda S, Stein RS, Richards-Dinger K, Bozkurt S (2005) Forecasting the evolution of seismicity in southern California: animations built on earthquake stress transfer. J Geophys Res 110:B05S16, doi:10.1029/2004JB003415

  • Tselentis G, Zahradnik J (2000) The Athens earthquake of 7 September 1999. Bull Seismol Soc Am 90:1143–1160

    Article  Google Scholar 

  • Wiemer S (2001) A software package to analyse seismicity: ZMAP. Seismol Res Lett 72(2):374–383

    Google Scholar 

  • Yaltirak 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(1–2):351–366. doi:10.1016/S0025-3227(02)00354-7

    Article  Google Scholar 

Download references

Acknowledgments

We thank the NOA Analysis group for phase picking. The open-source software GMT http://www.soest.hawaii.edu/gmt/ was used to make figures. We thank Dr. Mehmet Yilmazer for his help with KOERI data. We also thank Sean Ford, Thomas Braun and one anonymous reviewer for comments and suggestions. The relocated catalog is available upon request.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Athanassios Ganas.

Appendix

Appendix

The moment tensor solutions for the 14 events in Table 1, as computed using a time-domain moment tensor inversion method, are shown in detail. For each solution, we present the comparison between observed and synthetic waveforms (continuous and dashed lines, respectively) at the inverted stations. For each station, comparisons are shown for the radial, tangential and vertical components. To the left of each plot, we present a summary of the solution and the corresponding beach ball. Numbering of the solutions is as in Table 1.

figure a
figure b
figure c
figure d
figure e
figure f
figure g

Rights and permissions

Reprints and permissions

About this article

Cite this article

Ganas, A., Roumelioti, Z., Karastathis, V. et al. The Lemnos 8 January 2013 (M w = 5.7) earthquake: fault slip, aftershock properties and static stress transfer modeling in the north Aegean Sea. J Seismol 18, 433–455 (2014). https://doi.org/10.1007/s10950-014-9418-3

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s10950-014-9418-3

Keywords

Navigation