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. |
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Copyright © The Author(s), 2013. Published by Science Publishing Group |
Earthquake; Strain Energy; Energy Seismic Waves; Comparison
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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
@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 -