Abstract
Frequency-magnitude distribution was investigated in Elazig city and the surrounding area (coordinates ranging from 38.1° N to 39° N for latitudes and 39° E to 40° E for longitude) to reveal the present-day crustal stress within the region. For this study, a complete set of 5603 earthquakes of Md ≥ 1 from 1 January 2000 to 31 August 2020 were localized from the Bogazici University, Kandilli Observatory and Earthquake Research Institute, Regional Earthquake-Tsunami Monitoring Center (KOERI) catalogue. For the whole study region, spatial mapping of the frequency-magnitude distribution was thus produced. The frequency-magnitude distribution (b-value) for seismicity within the study area was not homogeneous. Outstanding variations in the b-value were detected with b ranging from b ≈ slightly more than 0.3–2. In this region, low b-values are mostly dominant in the region except for a few local areas. This study also shows that accumulated stresses are high particularly at the Pütürge segment in contrast to the fault drawn in the south, which represents the main thrust belt that runs through Hani-Lice and stretches to Çüngüş. As expected, stress accumulation in reverse faults is fairly higher. However, the sharing of the tension formed in the compression zone of the Arabian Plate and the Anatolian plate (i.e. stress partitioning in a sense), results in a low share in the reverse fault belt.
Similar content being viewed by others
Data availability
The earthquake data are public data from Bogazici University, Kandilli Observatory and Earthquake Research Institute, Regional Earthquake-Tsunami Monitoring Center (KOERI-RETMC) catalogue, and T.C. Prime Ministry Disaster and Emergency Management. Derived data supporting the findings of this study are available from the corresponding author Dr. Gulten Polat on request.
Code availability
In this study, ZMAP and Matlab (2019) were used. ZMAP is accessible via this link: SED|ZMAP (ethz.ch).
References
Aki K (1965) Maximum likelihood estimate of b in the formula log N = a − bM and its confidence limits. Tokyo Univ Bull Earthq Res Inst 43:237–239
Aki K (1981) A probabilistic synthesis of precursory phenomena. In: Simpson DW, Richards PG (eds) Earthquake prediction: an international review, Maurice Ewing Series 4. American Geophysical Union, Washington, D.C., pp 566–574
Akinci A, Antonioli A (2013) Observations and stochastic modeling of strong ground motions for the 2011 October 23 Mw 7.1 Van, Turkey, earthquake. Geophys J Int 192(3):1217–1239
Aksoy E, İnceöz M, Koçyiğit A (2007) Lake Hazar basin: a negative fower structure on the east Anatolian fault system (EAFS), SE Turkey. Turk J Earth Sci 16:319–338
Al-Lazki A, Seber D, Sandvol E, Türkelli N, Mohamad R, Barazangi M (2003) Tomographic Pn velocity and anisotropy structure beneath the Anatolian plateau (eastern Turkey) and the surrounding regions. Geophys Res Lett 30:24
Allen JRL (1986) Earthquake magnitude-frequency, epicentral distance and soft sediment deformation in sedimentary basins. Sed Geol 46:67–75. https://doi.org/10.1016/0037-0738(86)90006-
Bayrak E, Yilmaz Ş, Softa M, Türker T, Bayrak Y (2015) Earthquake hazard analysis for East Anatolian Fault Zone, Turkey. Nat Hazards 76:1063–1077
Bogazici University, Kandilli Observatory and Earthquake Research Institute, Regional Earthquake-Tsunami Monitoring Center (KOERI), from http://www.koeri.boun.edu.tr
Bora DK, Borah K, Mahanta R, Borgohain JM (2018) Seismic b-values and its correlation with the seismic moment and Bouguer gravity anomaly over Indo-Burma ranges of northeast India: tectonic implications. Tectonophysics 728–729:130–141. https://doi.org/10.1016/j.tecto.2018.01.001 (ISSN 0040-1951)
Bozkurt E (2001) Neotectonics of Turkey-a synthesis. Geodin Acta 14:3–30
Büyüksaraç A (2007) Investigation into the regional wrench tectonics of inner East Anatolia (Turkey) using potential field data. Phys Earth Planet Inter 160:86–95
Cambaz MD, Turhan F, Yılmazer M, Kekovalı K, Necmioğlu Ö, Kalafat D (2019) A review on kandilli observatory and earthquake research institute (KOERI) seismic network and earthquake catalog: 2008–2018. Adv Geosci 51:15–23. https://doi.org/10.5194/adgeo-51-15-2019
Çolak S, Aksoy E, Koçyiğit A, İnceöz M (2012) The Palu-Uluova strike-slip basin in the east Anatolian fault system, Turkey: its transition from the palaeotectonic to neotectonic stage. Turk J Earth Sci 21:1–24
Dewey JF, Şengör AMC (1979) Aegean and surrounding regions: complex multi-plate and continuum tectonics in a convergent zone. Geol Soc Am Bull 90:84–92
Duman TY, Emre Ö (2013) The east Anatolian fault: geometry, segmentation and jog characteristics. Geol Soc Lond Spec Publ 372(1):495–529
El-Isa ZH, Eaton DW (2014) Spatiotemporal variations in the b-value of earthquake magnitude-frequency. Tectonophysics 615:1–11
Frohlich C, Davis SD (1993) Teleseismic b values; or, much ado about 1.0. J Geophys Res 98:631–644
Göncüoğlu MC (2010) Introduction to the geology of Turkey: geodynamic evolution of the pre-alpine and alpine terranes. MTA Monographs Series 5 pp 66
Gutenberg R, Richter CF (1942) Earthquake magnitude, intensity, energy, and acceleration. Bull Seismol Soc Am 32:163–191. https://doi.org/10.1785/BSSA0320030163
Hempton MR (1987) Constraints on Arabian plate motion and extensional history of the Red Sea. Tectonics 6:687–705
Hempton MR, Dunne LA (1984) Sedimentation in pullapart basins: active examples in Eastern Turkey. J Geol 92:513–530
Hempton MR, Dunne LA, Dewey JF (1983) Sedimentation in an active strike- slip basin, south-eastern Turkey. J Geol 91:401–412
Jackson J (1994) Active tectonics of the Aegean region. Annu Rev Earth Planet Sci 22(1):239–271
Jiu X, Glacidogna G (2011) Spatial variation of seismic b-values distribution in China. Appl Mech Mater 71–78:4819–4822
Kalafat D (2015) Türkiye ve Çevresi Faylanma Kaynak Parametreleri (MT) Kataloğu (1938–2015); A cataloque of source parameters of moderate and strong earthquakes for Turkey and its surrounding area (1938–2015), İstanbul
Kalafat D (2016) Statistical evaluation of Turkey earthquake data (1900–2015): a case study. East Anatol J Sci 2:14–36
Kalafat D, Suvarıklı M, Öğütcü Z, Kekovalı K, Güneş Y, Yılmazer M, Çomoğlu M, Tunç S, Çok Ö (2013) KRDAE Türkiye Deprem Ağının Gelişimi: Bütünleşik Sismik Ağ Tasarımı/Development of KOERI Turkey Seismic Network: Integrated Seismic Network Design, 2.Türkiye Deprem Mühendisliği ve Sismoloji Konferansı Özetler Kitabı/2nd Turkey Earthquake Engineering and Seismology Conference Abstracts Book, s. 32–33, 25–27 Eylül 2013, Mustafa Kemal Üniversitesi, Tayfur Sökmen Kampüsü, Hatay
Katsumata K (2006) Imaging the high b-value anomalies within the subducting Pacific plate in the Hokkaido corner. Earth Planets Sp 58:49–52
Ketin I (1966) Tectonic units of Anatolia. Maden Tetkik ve Arama Bulletin, pp 23–34
Khan P, Chakraborty P (2007) The seismic b-value and its correlation with Bouguer gravity anomaly over the Shillong Plateau area: tectonic implications. J Asian Earth Sci 29:136–147. https://doi.org/10.1016/j.jseaes.2006.02.007
Koçyiğit A (1989) Suşehri basin: an active fault-wedge basin on the north Anatolian fault zone, Turkey. Tectonophysics 167:11–29
Koçyiğit A, Rojay B, Cihan M, Özacar A (2001) The June 6, 2000, Orta (Çankırı, Turkey) earthquake: sourced from a new antithetic sinistral strike-slip structure of the North Anatolian fault system, the Dodurga fault zone. Turk J Earth Sci 10:69–82
Koçyiğit A, Aksoy E, İnceöz M (2003) Basic Neotectonic characteristics of the Sivrice fault zone in the Sivrice-Palu area, East Anatolian fault system (EAFS), Turkey. Excursion Guide Book, International Workshop on the North Anatolian, East Anatolian and Dead Sea Fault Systems: Recent Progress in Tectonics and Palaeosismology, METU, Ankara, Turkey
Koeri data, the KOERI data is accessible via www.koeri.boun.edu.tr/sismo/2/tr/
Le Pichon X, Chamot-Rooke N, Lallemant S, Noomen R, Veis G (1995) Geodetic determination of the kinematics of central Greece with respect to Europe: implications for eastern Mediterranean tectonics. J Geophys Res 100:12675–12690
MATLAB (2019) The MathWorks, Inc., Natick, Massachusetts, United States
McKenzie DP (1972) Active tectonics of the Mediterranean region. Geophys J Royal Astronom Soc 30:109–185
Mogi K (1967) Earthquakes and fractures. Tectonophysics 5:35–55
Moreno DG, Hubert-Ferrari A, Moernaut J, Fraser JG, Boes X, Van Daele M, Avsar U, Çağatay N, De Batist M (2011) Structure and recent evolution of the Hazar Basin: a strike-slip basin on the East Anatolian Fault, Eastern Turkey. Basin Res 23:191–207. https://doi.org/10.1111/j.1365-2117.2010.00476.x
Mousavi SM (2017a) Mapping seismic moment and b-value within the continental collision orogenic-belt region of the Iranian Plateau. J Geodyn 103:26–41
Mousavi SM (2017b) Spatial variation in the frequency-magnitude distribution of earthquakes under the tectonic framework in the Middle East. J Asian Earth Sci 147:193–209
Mousavi SM, Ogwari PO, Horton SP, Langston CA (2017) Spatio-temporal evolution of frequency-magnitude distribution and seismogenic index during initiation of induced seismicity at Guy-Greenbrier, Arkansas. Phys Earth Planet Inter 267:53–66
Okay AI (2008) Geology of Turkey: a synopsis. Anschnit 2:19–42
Reilinger RE, McClusky SC, Oral MB, King RW, Toksoz MN (1997) Global positioning system measurements frequency-magnitude of present-day crustal movements in the Arabia–Africa–Eurasia plate collision zone. J Geophys Res 102(B5):9983–9999
Sancar T, Akyüz H (2014) Kuzey Anadolu Fay Zonu, Ilıpınar Segmenti’nin (Karlıova, Bingöl) Paleosismolojisi. Türkiye Jeoloji Bülteni 57(2):35–52
Şaroğlu F, Emre Ö, Kuşçu İ (1992) Active fault map of Turkey at Scale 1:1 000 000. Mineral Research and Explorations Institute of Turkey Publication, Ankara, 3 sheets
Scholz CH (1968a) Microfracturing and the inelastic deformation of rock in compression. J Geophys Res 73(4):1417–1432
Scholz CH (1968b) The relation of microfracturing in rock and its relation to earthquakes. Bull Seismol Soc Am 58:399–415
Schorlemmer D, Wiemer S, Wyss M (2005) Variations in earthquake-size distribution across different stress regimes. Nature 437:539–542
Senatorski P (2019) Gutenberg–Richter’s b value and earthquake asperity models. Pure Appl Geophys. https://doi.org/10.1007/s00024-019-02385-z
Şengör AMC, Yılmaz Y (1981) Tethyan evolution of Turkey: a plate tectonic approach. Tectonophysics 75:181–241
Tatar O, Piper JDA, Gürsoy H, Temiz H (1996) Regional significance of Neotectonic counter-clockwise rotation in central Turkey. Int Geol Rev 38:692–700
Utsu T (1965) A method for determining the value of b in the formula logN=a-bM showing the magnitude-frequency relation for earthquakes. Geophys Bull Hokkaido Univ 13:99–103 (in Japanese with English abstract)
Warren NW, Latham GV (1970) An experiment study of thermal induced microfracturing and its relation to volcanic seismicity. J Geophys Res 75:4455–4464
Wessel P, Smith WHF, Scharroo R, Luis JF, Wobbe F (2013) Generic mapping tools: improved version released. EOS Trans AGU 94:409–410
Westaway R, Arger J (1996) The Gölbaşı basin, southeasternTurkey: a complex discontinuity in a major strike-slip fault zone. J Geol Soc Lond 153:729–744
Wiemer S (2001) A software package to analyze seismicity: ZMAP. Seismol Res Lett 72:373–382
Wiemer S, Wyss M (1997) Mapping the frequency—magnitude distribution in asperities: an improved technique to calculate recurrence times? J Geophys Res 102:15115–15128
Wiemer S, Wyss M (2000) Minimum magnitude of completeness in earthquake catalogs: examples from Alaska, the western US and Japan. Bull Seism Soc Am 90:859–869
Wiemer S, McNutt SR, Wyss M (1998) Temporal and three-dimensional spatial analyses of the frequency-magnitude distribution near Long Valley Caldera, California. Geophys J Int 134:409–421
Woessner J, Wiemer S (2005) Assessing the quality of earthquake catalogues: estimating the magnitude of completeness and its uncertainty. Bull Seismol Soc Am. https://doi.org/10.1785/012040007
Wyss M (1973) Towards a physical understanding of the earthquake frequency distribution. Geophys J Roy Astron Soc 31(4):34
Acknowledgements
I would like to thank all the staff at KOERI-RETMC for providing data. Also, I am grateful to Dr. Doğan Kalafat from KOERI for his valuable comments regarding seismic analysis of the study region. Some figures in the paper were created using the GMT software package (Wessel et al. 2013) and MATLAB19b. I thank the anonymous referees for their useful suggestions.
Funding
This study has not been supported by any projects or/and institutions. This research did not receive any specific grant from funding agencies in the public, commercial, or not-for-profit sectors.
Author information
Authors and Affiliations
Corresponding author
Ethics declarations
Conflict of interest
All authors declare that they have no conflicts of interest.
Human and animal rights
No animals and human participants were involved in this study.
Additional information
Communicated by Dr. Aybige Akinci (ASSOCIATE EDITOR) / Prof. Ramon Zúñigas (CO-EDITOR-IN-CHIEF).
The original online version of this article was revised: uncomplete information for communicated by.
Rights and permissions
About this article
Cite this article
Polat, G. Spatial analysis of b-value variability in Elazig city and the surrounding area (Eastern Turkey). Acta Geophys. 70, 15–25 (2022). https://doi.org/10.1007/s11600-021-00694-3
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s11600-021-00694-3