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GSHAP revisited for the prediction of maximum credible earthquake in the Sikkim region, India

Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Global Seismic Hazard Assessment Program (GSHAP) has classified the Indian peninsula into several seismogenic zones. Considering the seismotectonic setting of the Sikkim Himalaya, sources 2, 3, 4, 5, 25, 26, 27 and 86 may be critical in contributing to the seismic hazard of the region. These seismogenic zones have been classified as Himalayan source (25, 86), extension of Tibetan plateau (26, 27), Burmese arc subduction zone (4, 5), Shillong plateau (3) and the Indian Shield region (2). The probabilistic seismic hazard assessment of the region necessitated prediction of Maximum Credible Earthquake magnitude for each source with 10% probability of exceedance in 50 years. Considering the widespread damages caused in the state capital of Sikkim due to the recent earthquakes of 1934 (Mw = 8) and 1988 (Mw = 7.2) a 50-year prediction seemed to be reasonable. Gutenberg-Richter (b-value) approach and Gumbel's method of extreme value statistics have been used in the present analysis for the prediction of Maximum Credible Earthquake magnitude, results of both being comparable to each other. The maximum credible earthquake magnitude as predicted by both the methods are above 6 except for zone 26, the highest being in the Burmese arc with a magnitude of 8.5 by Gutenberg-Richter approach and a magnitude of 7.7 by Gumbel's method.
Słowa kluczowe
Rocznik
Strony
143--152
Opis fizyczny
Bibliogr. 19 poz.
Twórcy
autor
  • Department of Geology and Geophysics, Indian Institute of Technology, Kharagpur - 721302, India
autor
  • Department of Geology and Geophysics, Indian Institute of Technology, Kharagpur - 721302, India
autor
  • Department of Geology and Geophysics, Indian Institute of Technology, Kharagpur - 721302, India
autor
  • Department of Geology and Geophysics, Indian Institute of Technology, Kharagpur - 721302, India
autor
  • Department of Geology and Geophysics, Indian Institute of Technology, Kharagpur - 721302, India
Bibliografia
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  • Bhatia, S.C., M. Ravi Kumar and H.K. Gupta, 1999, A probalistic seismic hazard map of India and adjoining regions, Ann. di Geofis. 42, 6, 1153-1166.
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  • Gumbel, E.J., 1958, Statistics of Extremes, Columbia University Press, New York.
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  • Gutenberg, B., and C.F. Richter, 1954, Seismicity of Earth and Associated Phenomena, Princeton University Press, Princeton NJ.
  • Khattri, K.N., 1987, Great earthquakes, seismicity gaps and potential for earthquake disaster along the Himalaya plate boundary. In: K. Mogi and K.N. Khattri (eds.), "Earthquake Prediction", Tectonophysics 138, 79-92.
  • Khattri, K.N., A.lVl. Rogers, D.M. Perkins and S.T. Algermissen, 1984, A seismic hazard map of India and adjacent areas, Tectonophysics 108, 93-134.
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  • Mukhopadhyay, M., and S. Dasgupta, 1988, Deep structure and tectonics of the Burmese arc: constraints from earthquake and gravity data, Tectonophysics 149, 299-322.
  • Ni, J.F., M.G. Speziale, M. Bevis, W.E. Holt, T.C. Wallace and W.R. Seager, 1989, Accretionary tectonics of Burma and the three dimensional geometry of the Burma subduction. Geology 17, 68-71.
  • Ponce, V.M., 1989, Engineering Hydrology, Principles and Practices, Prentice Hall, Engle-wood Cliffs, NJ.
  • Sykes, L.R., and S.C. Jaume, 1990, Seismic activity on neighbouring faults as a long-term pre¬cursor to large earthquakes in the San Francisco Bay area. Nature 348, 595-599.
  • Sykes, L.R., E.S. Bruce and C.H. Scholz, 1999, Rethinking earthquake prediction, Pageoph 155, 207-232.
  • Utsu, T., 2002, Statistical features of seismicity. In: W.H.K. Lee, H. Kanamori, P.C. Jennings and C. Kisslinger (eds.), "International Handbook of Earthquake and Engineering
  • Seismology", International Geophysics Series 81 A, 719-732, Amsterdam-Boston, Academic Press.
  • Verma, R.K., M. Mukhopadhyay and M.S. Ahluwalia, 1976, Earthquake mechanisms and tectonic features of northern Burma, Tectonophysics 32, 387-399.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BSL7-0009-0012
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