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Non-extensive framework for earthquakes: the role of fragments

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Języki publikacji
EN
Abstrakty
EN
The inclusion of fragment-asperity interaction inside tectonic plates to find a frequency magnitude relation for earthquakes, and the need for non-extensive statistics in this case is exposed. The usefulness of this formulation is shown. A comparison with seismic observations is also discussed.
Słowa kluczowe
Czasopismo
Rocznik
Strony
526--534
Opis fizyczny
Bibliogr. 23 poz.
Twórcy
Bibliografia
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  • Abe, S. (2010), Essential discreteness in generalized thermostatistics with nonlogarithmic entropy, EPL 90, 5, 50004, DOI: 10.1209/0295-5075/90/50004.
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  • Bagci, G.B., T. Oikonomou, and U. Tirnakli (2010), Comment on “Essential discreteness in generalized thermostatistics with non-logarithmic entropy” by S. Abe, arXiv:1006.1284v2 [cond-mat.stat-mech].
  • Bak, P. (1996), How Nature Works: The Science of Self-Organised Criticality, Copernicus Press, New York.
  • Burridge, R., and L. Knopoff (1967), Model and theoretical seismicity, Bull Seismol. Soc. Am. 57, 3, 341-371.
  • Cabo, A. (2010), Is the Tsallis q-mean value instable?, arXiv:1010.5825v1 [condmat. stat-mech].
  • De Rubeis, V., R. Hallgass, V. Loreto, G. Paladin, L. Pietronero, and P. Tosi (1996), Self-affine asperity model for earthquakes, Phys. Rev. Lett. 76, 14, 2599-2602, DOI: 10.1103/PhysRevLett.76.2599.
  • Englman, R., N. Rivier, and Z. Jaeger (1987), Fragment-size distribution in disintegration by maximum-entropy formalism, Philos. Mag. B 56, 6, 751-769, DOI: 10.1080/13642818708215309.
  • Gutenberg, B., and C.F. Richter (1944), Frequency of earthquakes in California, Bull. Seimol. Soc. Am. 34, 4, 185-188.
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  • Lomnitz-Adler, J., and C. Lomnitz (1979), A modified form of the Gutenberg–Richter magnitude-frequency relation, Bull. Seismol. Soc. Am. 69, 4, 1209-1214.
  • Matsushita, M. (1985), Fractal viewpoint of fracture and accretion, J. Phys. Soc. Jpn. 54, 857-860, DOI: 0.1143/JPSJ.54.857.
  • Olami, Z., H.J.S. Feder, and K. Christensen (1992), Self-organized criticality in a continuous, nonconservative cellular automaton modeling earthquakes, Phys. Rev. Lett. 68, 8, 1244-1247, DOI: 10.1103/PhysRevLett.68.1244.
  • Sarlis, N.V., E.S. Skordas, and P.A. Varotsos (2010), Nonextensivity and natural time: The case of seismicity, Phys. Rev. E 82, 2, 021110, DOI: 10.1103/PhysRevE.82.021110.
  • Silva, R., G.S. França, C.S. Vilar, and J.S. Alcaniz (2006), Nonextensive models for earthquakes, Phys. Rev. E 73, 026102, DOI: 10.1103/PhysRevE.73.026102.
  • Sotolongo-Costa, O., and A. Posadas (2004), Fragment-asperity interaction model for earthquakes, Phys. Rev. Lett. 92, 4, 048501, DOI: 10.1103/PhysRevLett. 92.048501.
  • Sotolongo-Costa, O., E. Lopez-Pages, F. Barreras-Toledo, and J. Marin-Antuña (1994), Scaling in drop distributions: An application in combustion, Phys. Rev. E 49, 5, 4027-4030, DOI: 10.1103/PhysRevE.49.4027.
  • Sotolongo-Costa, O., Y. Moreno-Vega, J.J. Lloveras-González, and J.C. Antoranz (1996), Criticality in droplet fragmentation, Phys. Rev. Lett. 76, 1, 42-45, DOI: 10.1103/PhysRevLett.76.42.
  • Telesca, L., and C.-C. Chen (2010), Nonextensive analysis of crustal seismicity in Taiwan, Nat. Hazards Earth Syst. Sci. 10, 1293-1297, DOI: 10.5194/nhess-10-1293-2010.
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Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BSL4-0017-0003
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