This paper describes a technique for determining the potential energy of deformed material around a future earthquake rupture, with this energy being stored during the precursory period. The basic parameters are the following: rupture length on the Earth’s surface after the earthquake has occurred , rupture depth h, and the relative block movement along the rupture strike line . We compared the results for 44 large earthquakes with those derived by determining seismic wave energy from earthquake magnitude.
| Published in | Earth Sciences (Volume 2, Issue 2) |
| DOI | 10.11648/j.earth.20130202.14 |
| Page(s) | 47-57 |
| Creative Commons |
This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited. |
| Copyright |
Copyright © The Author(s), 2013. Published by Science Publishing Group |
Earthquake; Strain Energy; Energy Seismic Waves; Comparison
| [1] | J.N. Brune, The Physics of Earthquake Strong Motion, in Lomnitz, C. and Rosenblueth, E., Eds., Seismic Risk and Engineering Decisions, New York: Elsevier Sci. Publ. Co., 1976, pp.141-177. |
| [2] | C. Lomnitz, and K.S. Singh, Earthquakes and Earthquake Prediction, in Lomnitz, C. and E. Rosenblueth, , Eds., Seis¬mic Risk and Engineering Decisions, New York: Elsevier Sci. Publ. Co., 1976, pp. 3-30 |
| [3] | J. Rice, Ed., The Mechanics of Earthquake Rupture, Ams-terdam: Elsevier, 1982. |
| [4] | K. Kasahara, Earthquake Mechanics, Cambridge Univer¬sity Press, 1981. |
| [5] | S.S. Grigoryan, On the Mechanics of Earthquake Genera¬tion and the Meaning of Empirical Relations in Seismology, Dokl. ANSSSR, 1988, vol. 299, no. 5, pp. 1094-1101. |
| [6] | Ch. Richter, Elementary Seismology, San Francisco: W.H. Freeman and Company, 1958. |
| [7] | B. Gutenberg, and C.F. Richter, Earthquake Magnitude, Intensity, and Acceleration, Bull. Seismol. Soc. Amer., 1956, vol. 46, no. 2, pp. 105-145. |
| [8] | H. Jeffreys, The Earth, Cambridge University Press, 1970. |
| [9] | N.N. Ambraseys, MaximUm Intensity of GroUnd Movements Caused by Faulting, Proc. 4th World Conf. Earthq. Eng., vol. 1, A-2, pp. 154-171, Santiago, Chile, 1969. |
| [10] | D. McKenzie, and J.N. Brune, Melting on Fault Planes during Large Earthquakes, Geophys. J. R. Astr. Soc., 1972, vol. 29, pp. 65-78. |
| [11] | S.P. Timoshenko, and J. Goudier, Theory of Elasticity. 2nd ed., New York: McGraw-Hill, 1951. |
| [12] | H.F. Reid, The Elastic Rebound Theory of Earthquakes, Univ, Calif. Publ. Bull. Dept. Geol., 1911, no.6. |
| [13] | D.L. Wells, and K.I. Coppersmith, New Empirical Rela¬tionship among Magnitude, Rupture Length, Rupture Width, Rupture Area, and Surface Displacement, Bull. Seismol. Soc. Amer., 1994, vol. 84, no. 4, pp. 974-1002. |
| [14] | T. Rikitake, Earthquake Prediction, Amsterdam: Elsevier, 1976. |
| [15] | L. Knopoff, Energy Release in Earthquakes, Geophys. J., 1958, vol. 1, no. 1, pp. 44-52. |
| [16] | K. Mogi, Earthquake Prediction, Academic Press, 1985. |
APA Style
E. E. Khachiyan. (2013). Method for Determining the Potential Strain Energy Stored in the Earth before a Large Earthquake. Earth Sciences, 2(2), 47-57. https://doi.org/10.11648/j.earth.20130202.14
ACS Style
E. E. Khachiyan. Method for Determining the Potential Strain Energy Stored in the Earth before a Large Earthquake. Earth Sci. 2013, 2(2), 47-57. doi: 10.11648/j.earth.20130202.14
AMA Style
E. E. Khachiyan. Method for Determining the Potential Strain Energy Stored in the Earth before a Large Earthquake. Earth Sci. 2013;2(2):47-57. doi: 10.11648/j.earth.20130202.14
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Download@article{10.11648/j.earth.20130202.14,
author = {E. E. Khachiyan},
title = {Method for Determining the Potential Strain Energy Stored in the Earth before a Large Earthquake},
journal = {Earth Sciences},
volume = {2},
number = {2},
pages = {47-57},
doi = {10.11648/j.earth.20130202.14},
url = {https://doi.org/10.11648/j.earth.20130202.14},
eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.earth.20130202.14},
abstract = {This paper describes a technique for determining the potential energy of deformed material around a future earthquake rupture, with this energy being stored during the precursory period. The basic parameters are the following: rupture length on the Earth’s surface after the earthquake has occurred , rupture depth h, and the relative block movement along the rupture strike line . We compared the results for 44 large earthquakes with those derived by determining seismic wave energy from earthquake magnitude.},
year = {2013}
}
TY - JOUR T1 - Method for Determining the Potential Strain Energy Stored in the Earth before a Large Earthquake AU - E. E. Khachiyan Y1 - 2013/04/02 PY - 2013 N1 - https://doi.org/10.11648/j.earth.20130202.14 DO - 10.11648/j.earth.20130202.14 T2 - Earth Sciences JF - Earth Sciences JO - Earth Sciences SP - 47 EP - 57 PB - Science Publishing Group SN - 2328-5982 UR - https://doi.org/10.11648/j.earth.20130202.14 AB - This paper describes a technique for determining the potential energy of deformed material around a future earthquake rupture, with this energy being stored during the precursory period. The basic parameters are the following: rupture length on the Earth’s surface after the earthquake has occurred , rupture depth h, and the relative block movement along the rupture strike line . We compared the results for 44 large earthquakes with those derived by determining seismic wave energy from earthquake magnitude. VL - 2 IS - 2 ER -
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