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Prediction of seismicity cycles in the Himalayas using artificial neural network

Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
In this paper, cyclic behaviour of seismicity cycles in the Himalayas has been exploited to predict the future earthquake activity using Artificial Neural Network (ANN). The Himalayan region has been divided into six seismogenic zones. A feed forward multi-layer ANN has been used to evaluate the seismicity fluctuation in the time series containing data from historical times to 1998 for each zone. The most widely used Back Propagation Algorithm (BPA) is applied to train the neural network. BPA iteratively minimises an error function over the network outputs and a set of target outputs taken from the training data set. The results show that the probability of occurrence of moderate to great earthquake in next 50 years is relatively lower in the Hindukush-Pamirs zone. Since the intense release of energy will take place in the Kashmir-Himachal Pradesh zone, between 2030 to 2055, the probability of occurrence of moderate to great earth-quake is higher. The accumulation of energy stage is still going on in the India -Western Nepal Border zone, and there will be an increase in seismic activity after 2030 for the next 50 years. The hazard parameters could not be estimated for the Nepal-India-Sikkim Border zone because of lesser number of data to capture cyclic behaviour. In NE India, intense release and remnant release will take place up to 2030 due to which there will be an increase in the probability of occurrence of moderate to great earthquake in this zone. In Burma-Andaman Nicobar, the energy accumulation stage for the next cycle has started in 1990 and will continue till 2020.
Rocznik
Strony
299--309
Opis fizyczny
Bibliogr. 17 poz.
Twórcy
autor
  • Department of Earthquake Engineering, Indian Institute of Technology, Roorkee-247 667, India
autor
  • Department of Civil Engineering, Indian Institute of Technology Roorkee-247 667, India
Bibliografia
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  • Drakopoulos, J.C., and H.N. Srivastava, 1972, The dependence of earthquake frequency magnitude relationship and strain energy release upon the focal depth in Hindukush region, Ann. di Geofis. 23, 593-606.
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  • Gupta, G.D., and H.N. Srivastava, 1990, On earthquake risk assessment in the Himalayan region, Memoir Geological Society of India 23, 173-199.
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  • Rao, S.P., and R.B. Rao, 1979, Estimated earthquake probabilities in north-east India, Andaman-Nicobar Island, Mausam 30, 267-273.
  • Reid, H.F., 1910, The mechanics of the earthquake. In: "The California Earthquake of April 11, 1906. Report of the State Earthquake Investigation Commission", 2, Carnegie Institution, Washington D.C.
  • Richards, J.A., 1999, Remote Sensing and Digital Image Analysis: An Introduction, 2nd ed. Springer-Verlag, Berlin.
  • Rumelhart, D.E., and J.L. McClelland, 1986, Parallel Distributed Processing, vol. 2, MIT Press, Cambridge, MA.
  • Schalkoff, R.J., 1997, Pattern Recognition: Statistical, Structural and Neural Approaches, Wiley and Sons Inc., New York.
  • Serpico, S.B., and P. Roli, 1995, Classification of multisensor remote sensing images by structural neural networks, IEEE Trans. Geosci. Rem. Sens. 33, 3, 562-577.
  • Shanker, D., and M.L. Sharma, 1998, Estimation of Seismic Hazard Parameters for the Himalayas and its Vicinity from Complete Data Files, Pure Appl. Geophys. 152, 267-279.
  • Sharma, M.L., and D. Shanker, 2001, E.stimation of seismic hazard parameters for the Himala¬yas and its vicinity from mix data files, ISET J. Earthq. Techn. 38, 2-4, 93-102.
  • Sharma, M.L., H.R. Wason and R. Dimri, 2003, Seismic zonation of the Delhi region for bedrock ground motion. Pure Appl. Geophys. 160, 2281-2398.
  • Srivastava, H.N., 1973, The crustal seismicity and nature of faulting near India Nepal and Tibet trijunction. Him. Geol. 3, 381-393.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BSL7-0009-0035
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