First evidence of the non extensive character of pre and post seismic deformation of Samos (2020) Mw7.0 earthquake

Vallianatos, Filippos; Michas, Georgios; Sakkas, Vassilis; Partheniou, Eleni I.

doi:10.1007/s11600-021-00606-5

Artykuł - szczegóły

Tytuł artykułu

First evidence of the non extensive character of pre and post seismic deformation of Samos (2020) Mw7.0 earthquake

Autorzy

Vallianatos Filippos , Michas Georgios , Sakkas Vassilis , Partheniou Eleni I.

Wybrane pełne teksty z tego czasopisma

https://www.springer.com/journal/11600

Identyfikatory

DOI

10.1007/s11600-021-00606-5

Warianty tytułu

Języki publikacji

Abstrakty

The statistical patterns occurring on the threshold of an earthquake, in the transition stage immediately before and after the rupture, still remain unclear. Investigating the dynamical features of surface deformation a few days before and after the earthquake co-seismic rupture are crucial to understand the mechanics of the earthquake process. In the present work, we study surface displacements as estimated using continuous GNSS measurements in the vicinity of the 2020 Mw7.0 Samos (Greece) strong, shallow earthquake. The GNSS time series before and after the Mw7.0 earthquake in SAMO (belonging to METRICA SA HexagonSmartNet commercial network) station demonstrate signifcant surface deformation in the broader epicentral area. We further analyze the surface displacement increments a few days before and after the Samos Mw7.0 earth quake using the non-extensive statistical physics (NESP) framework, which could provide a frame to study the complexity of the earthquake process. The results of the analysis suggest that the statistical distribution of ground displacement increments presents asymptotic power-law behavior that deviates from the standard Gaussian function. Instead, the observed distributions can be described by the q-Gaussian function derived in the NESP framework, for q-values in the range of 1.10–1.15. In addition, the statistical pattern that was obtained from the analysis is further discussed in terms of superstatistics, indicating that the ground displacement increments a few days before and after the Mw7.0 earthquake correspond to a system with high enough degrees of freedom of the order of 13–15. Furthermore, for comparison, a four years record of continuous GNSS measurements was analyzed using NESP. The results support the non-extensive character of displacement increments using a four years period of recordings suggesting long-range temporal correlations.

Słowa kluczowe

CGNSS Tsallis entropy earthquake Samos surface deformation Q-Gaussian

CGNSS Entropia Tsallisa trzęsienie ziemi Samos deformacja powierzchni

Wydawca

Instytut Geofizyki PAN
Springer

Czasopismo

Acta Geophysica

Rocznik

2021

Tom

Vol. 69, no. 3

Strony

1127--1136

Opis fizyczny

Bibliogr. 63 poz.

Twórcy

autor

Vallianatos Filippos

fvallian@geol.uoa.gr

Section of Geophysics − Geothermics, Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, 15784 Panepistimiopolis, Athens, Greece
Institute of Physics of Earth’s Interior and Geohazards, UNESCO, Chair On Solid Earth Physics and Geohazards Risk Reduction, Hellenic Mediterranean University Research Center, Grete, Greece

autor

Michas Georgios

Section of Geophysics − Geothermics, Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, 15784 Panepistimiopolis, Athens, Greece
Institute of Physics of Earth’s Interior and Geohazards, UNESCO, Chair On Solid Earth Physics and Geohazards Risk Reduction, Hellenic Mediterranean University Research Center, Grete, Greece

autor

Sakkas Vassilis

Section of Geophysics − Geothermics, Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, 15784 Panepistimiopolis, Athens, Greece
Institute of Physics of Earth’s Interior and Geohazards, UNESCO, Chair On Solid Earth Physics and Geohazards Risk Reduction, Hellenic Mediterranean University Research Center, Grete, Greece

autor

Partheniou Eleni I.

Section of Geophysics − Geothermics, Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, 15784 Panepistimiopolis, Athens, Greece
Institute of Physics of Earth’s Interior and Geohazards, UNESCO, Chair On Solid Earth Physics and Geohazards Risk Reduction, Hellenic Mediterranean University Research Center, Grete, Greece

Bibliografia

1. Antonopoulos CG, Michas G, Vallianatos F, Bountis T (2014) Evidence of q-exponential statistics in Greek seismicity. Phys A 409:71–77. https://doi.org/10.1016/j.physa.2014.04.042
2. Aristotle University Of Thessaloniki Seismological Network (1981) Permanent Regional Seismological Network operated by the Aristotle University of Thessaloniki. Int Feder Digital Seism Netw. https://doi.org/10.7914/SN/HT
3. Beck C (2001) Dynamical foundations of non-extensive statistical mechanics. Phys Rev Lett 87(18):180601. https://doi.org/10.1103/PhysRevLett.87.180601
4. Beck C (2009) Recent developments in superstatistics. Brazilian J. Physics 39:357–363. https://doi.org/10.1590/S0103-97332009000400003
5. Beck C (2006) Superstatistical brownian motion. Prog Theor Phys Suppl 162:29–36. https://doi.org/10.1143/PTPS.162.29
6. Beck C, Cohen EGD (2003) Superstatistics. Phys A 322:267–275. https://doi.org/10.1016/S0378-4371(03)00019-0
7. Bogusz J, Klos A, Figurski M, Kujawa M (2015) Investigation of long-range dependencies in the stochastic part of daily gps solutions. Surv Rev. https://doi.org/10.1179/1752270615Y.0000000022
8. 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. https://doi.org/10.1016/j.tecto.2012.11.026
9. Dach R, Lutz S, Walser P, Fridez P (eds) (2015b) Bernese GNSS software version 5.2. User manual. Astronomical Institute, University of Bern, Bern Open Publishing. https://doi.org/10.7892/boris.72297
10. Efstathiou A, Tzanis A, Vallianatos F (2015) Evidence of non-extensivity in the evolution of seismicity along the San-Andreas Fault, California, USA: an approach based on tsallis statistical physics. Phys Chem Earth 85–86:56–68. https://doi.org/10.1016/j.pce.2015.02.013
11. Ferraro F, Koutalonis I, Vallianatos F, Agosta F (2019) Application of non-extensive Statistical Physics on the particle size distribution in natural carbonate fault rocks. Tectonophys 771:228219. https://doi.org/10.1016/j.tecto.2019.228219
12. Filatov D, Lyubushin A (2017) Fractal analysis of gps time series for early detection of disastrous seismic events. Phys A 469:718–730. https://doi.org/10.1016/j.physa.2016.11.046
13. Filatov D, Lyubushin A (2019) Precursory analysis of gps time series for seismic hazard assessment. Pure Appl Geophys 177:509–530. https://doi.org/10.1007/s00024-018-2079-3
14. Ganas Α (2020). NOAFAULTS KMZ layer Version 3.0 (2020 update) (Version V3.0). Zenodo. https://doi.org/10.5281/zenodo.4304613
15. Ganas A, Elias P, Briole P, Tsironi V, Valkaniotis S, Escartin J, Karasante I, Efstathiou E (2020) Fault responsible for Samos earthquake identified. Temblor. https://doi.org/10.32858/temblor.134
16. Jolivet L, Brun JP (2010) Cenozoic geodynamic evolution of the Aegean. Int J Earth Sci 99:109–138. https://doi.org/10.1007/s00531-008-0366-4
17. Keilis-Borok VI (1990) The lithosphere of the earth as a nonlinear system with implications for earthquake prediction. Rev Geophys 28(1):19–34. https://doi.org/10.1029/RG028i001p00019
18. Kiratzi A (2002) Stress tensor inversions along the westernmost north anatolian fault zone and its continuation into the North Aegean Sea. Geophys J Int 151(2):360–376. https://doi.org/10.1046/j.1365-246X.2002.01753.x
19. Kiratzi A (2014) Mechanisms of Earthquakes in Aegean. In: Beer M, Kougioumtzoglou IA, Patelli E, Siu-Kui AuI (eds) Encyclopedia of earthquake engineering. Springer, Berlin, pp 1–22
20. Klos A, Bogusz J, Figurski M, Kosek W (2014a) Uncertainties of geodetic velocities from permanent gps observations: the sudeten case study. Acta Geodyn Geomater 11 3(175):201–209. https://doi.org/10.13168/AGG.2014005
21. Klos A, Bogusz J, Figurski M, Kosek W (2014b) Irregular variations in gps time series by probability and noise analysis. Surv Rev. https://doi.org/10.1179/1752270614Y.0000000133
22. Klos A, Gruszczynska M, Bos MS, Boy J, Bogusz J (2019) Estimates of Vertical Velocity Errors for IGS ITRF2014 Stations by Applying the Improved Singular Spectrum Analysis Method and Environmental Loading Models. In: Braitenberg C, Rossi G (eds) Geodynamics and Earth Tides Observations from Global to Micro Scale. Pageoph Topical Volumes, Birkhäuser, Cham. https://doi.org/10.1007/978-3-319-96277-1_18
23. Koutalonis I, Vallianatos F (2017) Evidence of non-extensivity in earth’s ambient noise. Pure Appl Geophys 174:4369–4378. https://doi.org/10.1007/s00024-017-1669-9
24. Langbein J, Murray J, Snyder H (2006) Coseismic and initial postseismic deformation from the 2004 Parkfield, California, earthquake, Observed by global positioning system, electronic distance meter, creepmeters, and borehole strainmeters. Bul Seism Soc Am 96(4B):S304–S320. https://doi.org/10.1785/0120050823
25. Lekkas E et al (2020) The October 30, 2020, M 6 9 Samos (Greece) earthquake. Newsl Environ Disaster Cris Manag Strateg 92–93:1–156
26. Michas G, Vallianatos F, Sammonds P (2013) Non-extensivity and long-range correlations in the earthquake activity at the West Corinth rift (Greece). Nonlinear Proc Geophys 20:713–724. https://doi.org/10.5194/npg-20-713-2013
27. Michas G, Vallianatos F, Sammonds P (2015) Statistical mechanics and scaling of fault population with increasing strain in the Corinth Rift. Earth Planet Sci Lett 431:150–163. https://doi.org/10.1016/j.epsl.2015.09.014
28. Ozacar A (2011). Present day stress pattern of turkey from inversion of updated earthquake focal mechanism catalogue. AGU Fall Meeting Abstracts S21A-2156
29. Papadakis G, Vallianatos F, Sammonds P (2013) Evidence of nonextensive statistical physics behavior of the Hellenic subduction zone seismicity. Tectonophys 608:1037–1048. https://doi.org/10.1016/j.tecto.2013.07.009
30. Papadakis G, Vallianatos F, Sammonds P (2014) A nonextensive statistical physics analysis of the 1995 Kobe, Japan earthquake. Pure Appl Geophys 172:1923–1931. https://doi.org/10.1007/s00024-014-0876-x
31. Papadakis G, Vallianatos F, Sammonds P (2016) Non-extensive statistical physics applied to heat flow and the earthquake frequency distribution in Greece. Phys A 456:135–144. https://doi.org/10.1016/j.physa.2016.03.022
32. Papadimitriou P, Kapetanidis V, Karakonstantis A, Spingos I, Kassaras I, Sakkas V, Kouskouna V, Karatzetzou A, Pavlou K, Kaviris G, Voulgaris N (2020) First results on the M=6 9 Samos earthquake of 30 October 2020. Bull Geol Soc Greece. 56(1):251–279. https://doi.org/10.12681/bgsg.25359
33. Papanikolaou D (1997) The tectonostratigraphic terranes of the Hellenides. Annales Géologiques des Pays Helléniques 37:495–514
34. Reid HF (1910) The mechanics of the earthquake. The California Earthquake of April 18, 1906: report of the state earthquake investigation commission 2:16-18 Carnegie Institution of Washington Publication: Washington, DC, USA
35. Reilinger R, Ergintav S, Bürgmann R, McCluskey S, Lenk O, Barka A, Gurkan O, Hearn E, Feigl KL, Cakmak R et al (2000) Coseismic and postseismic fault slip for the 17 august 1999, M = 7.5, Izmit Turkey Earthquake. Science 289:1519–1524. https://doi.org/10.1126/science.289.5484.1519
36. Reilinger R et al (2006) GPS constraints on continental deformation in the Africa-Arabia-Eurasia continental collision zone and implications for the dynamics of plate interactions. J Geophys Res 111:B05411. https://doi.org/10.1029/2005JB004051
37. Ring U, Okrusch M, Will T (2007) Samos Island, Part I: metamorphosed and non metamorphosed nappes, and sedimentary basins. J Virtual Explor 27:5. https://doi.org/10.3809/jvirtex.2007.00180
38. Saltas V, Vallianatos F, Triantis D, Koumoudeli T, Stavrakas I (2019) Non-extensive statistical analysis of acoustic emissions series recorded during the uniaxial compression of brittle rocks. Phys A 528:121498. https://doi.org/10.1016/j.physa.2019.121498
39. Saltas V, Vallianatos F, Triantis D, Stavrakas I (2018) Complexity in laboratory seismology: from electrical and acoustic emissions to fracture. In: Chelidze T, Telesca L, Vallianatos F (eds) Complexity of seismic time series measurement and application. Elsevier, pp 239–273. https://doi.org/10.1016/B978-0-12-813138-1.00008-0
40. Sornette D (2006) Critical phenomena in natural sciences: chaos, fractals, selforganization and disorder: concepts and tools Springer Series of Synergetic. Springer, Berlin
41. Telesca L (2010) Analysis of Italian seismicity by using a nonextensive approach. Tectonophys 494:155–162. https://doi.org/10.1016/j.tecto.2010.09.012
42. Telesca L (2011) Tsallis-based nonextensive analysis of the Southern California Seismicity. Entropy 13:1267–1280. https://doi.org/10.3390/e13071267
43. Triantafyllou I, Gogou M, Mavroulis S, Lekkas E, Papadopoulos GA, Thravalos M. The Tsunami Caused by the 30 October 2020 Samos (Aegean Sea) Mw7.0 Earthquake: Hydrodynamic Features, Source Properties and Impact Assessment from Post-Event Field Survey and Video Records. Journal of Marine Science and Engineering. 2021; 9(1):68. https://doi.org/10.3390/jmse9010068
44. Tsallis C (1988) Possible generalization of Boltzmann-Gibbs statistics. J Stat Phys 52(1):479–487. https://doi.org/10.1007/BF01016429
45. Tsallis C (2009) Introduction to nonextensive statistical mechanics—approaching a complex world. Springer, New York. https://doi.org/10.1007/978-0-387-85359-8
46. Tserolas V, Mertikas SP, Frantzis X (2013) The western crete geodetic infrastructure: long-range power-law correlations in GPS time series using detrended fluctuation analysis. Adv Space Res 51:1448–1467
47. Tur H et al (2015) Pliocene-Quaternary tectonic evolution of the Gulf of Gökova, southwest Turkey. Tectonophys 638:158–176
48. Vallianatos F (2011) A non-extensive statistical physics approach to the polarity reversals of the geomagnetic field. Phys A 390:1773–1778
49. Vallianatos F, Sammonds P (2010) Is plate tectonics a case of non-extensive thermodynamics? Physica A 389:4989–4993
50. Vallianatos F, Pavlou K (2021) Scaling properties of the Mw7.0 Samos (Greece), 2020 aftershock sequence, Acta Geophysica. https://doi.org/10.1007/s11600-021-00579-5
51. Vallianatos F, Sammonds P (2011) A non-extensive statistics of the fault-population at the valles marineris extensional province, Mars. Tectonophys 509:50–54. https://doi.org/10.1016/j.tecto.2011.06.001
52. Vallianatos F, Sammonds P (2013) Evidence of non-extensive statistical physics of the lithospheric instability approaching the 2004 Sumatran-Andaman and 2011 Honshu mega-earthquakes. Tectonophys 590:52–58. https://doi.org/10.1016/j.tecto.2013.01.009
53. Vallianatos F, Benson P, Meredith P, Sammonds P (2012) Experimental evidence of a non-extensive statistical physics behavior of fracture in triaxially deformed etna basalt using acoustic emissions. Europhys Lett 97:58002. https://doi.org/10.1209/0295-5075/97/58002
54. Vallianatos F, Michas G, Benson P, Sammonds P (2013) Natural time analysis of critical phenomena: the case of acoustic emissions in triaxially deformed etna basalt. Phys A 392:5172–5178. https://doi.org/10.1016/j.physa.2013.06.051
55. Vallianatos F, Karakostas V, Papadimitriou E (2014) A Non-Extensive statistical physics view in the spatiotemporal properties of the 2003 (Mw62) Lefkada, Ionian Island Greece, aftershock sequence. Pure Appl Geophys 171(7):1343–1534. https://doi.org/10.1007/s00024-013-0706-6
56. Vallianatos F, Michas G, Papadakis G (2016a) A description of seismicity based on non-extensive statistical physics: A review. In: D’Amico S (ed) Earthquakes and their impact on society. Springer Natural Hazards. Springer, Heidelberg, pp 1–41
57. Vallianatos F, Michas G, Papadakis G (2016b) Generalized statistical mechanics approaches to earthquakes and tectonics. Proc R Roc A 472:20160497. https://doi.org/10.1098/rspa.2016.0497
58. Vallianatos F, Michas G, Papadakis G (2018) Nonextensive statistical seismology: an overview In: In: Chelidze T, Vallianatos F, Telesca (eds) Complexity of seismic time series. Elsevier, Amsterdam, pp 25–60
59. Vallianatos F, Michas G (2020) Complexity of fracturing in terms of non-extensive statistical physics: from earthquake faults to arctic sea ice fracturing. Entropy 22(11):1194. https://doi.org/10.3390/e22111194
60. Valverde-Esparza SM, Ramirez-Rojas A, Flores-Marquez EL (2012) Non-extensivity analysis of seismicity within four subduction regions in Mexico. Acta Geophys. 60:833–845. https://doi.org/10.2478/s11600-012-0012-1
61. Vilar CS, Franca GS, Silva R, Alcaniz JS (2007) Nonextensivity in geological faults? Phys A 377:285–290. https://doi.org/10.1016/j.physa.2006.11.017
62. Wang P, Chang Z, Wang H (2015) Lu H (2015) Scale-invariant structure of energy fluctuations in real earthquakes. Eur Phys J B 88:206. https://doi.org/10.1140/epjb/e2017-70702-y
63. Zumberge JF, Heflin MB, Jefferson DC, Watkins MM, Webb FH (1997) Precise point positioning for the efficient and robust analysis of GPS data from large networks. J Geophys Res 102(B3):5005–5017. https://doi.org/10.1029/96JB03860

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