том 167 издание 1-2 страницы 91-106

Omori’s Law Applied to Mining-Induced Seismicity and Re-entry Protocol Development

Тип публикацииJournal Article
Дата публикации2009-12-22
SCImago Q2
WOS Q2
БС2
SJR0.512
CiteScore4
Impact factor1.9
ISSN00334553, 14209136, 00334533
Geochemistry and Petrology
Geophysics
Краткое описание
This paper describes a detailed study of the Modified Omori’s law n(t) = K/(c + t) p applied to 163 mining-induced aftershock sequences from four different mine environments in Ontario, Canada. We demonstrate, using a rigorous statistical analysis, that this equation can be adequately used to describe the decay rate of mining-induced aftershock sequences. The parameters K, p and c are estimated using a uniform method that employs the maximum likelihood procedure and the Anderson–Darling statistic. To estimate consistent decay parameters, the method considers only the time interval that satisfies power-law behavior. The p value differs from sequence to sequence, with most (98%) ranging from 0.4 to 1.6. The parameter K can be satisfactorily expressed by: K = κN 1, where κ is an activity ratio and N 1 is the measured number of events occurring during the first hour after the principal event. The average κ values are in a well-defined range. Theoretically κ ≤ 0.8, and empirically κ ∈ [0.3–0.5]. These two findings enable us to develop a real-time event rate re-entry protocol 1 h after the principal event. Despite the fact that the Omori formula is temporally self-similar, we found a characteristic time T MC at the maximum curvature point, which is a function of Omori’s law parameters. For a time sequence obeying an Omori process, T MC marks the transition from highest to lowest event rate change. Using solely the aftershock decay rate, therefore, we recommend T MC as a preliminary estimate of the time at which it may be considered appropriate to re-enter an area affected by a blast or large event. We found that T MC can be estimated without specifying a p value by the expression: T MC = a N 1 , where a and b are two parameters dependent on local conditions. Both parameters presented well-constrained empirical ranges for the sites analyzed: a ∈ [0.3–0.5] and b ∈ [0.5–0.7]. These findings provide concise and well-justified guidelines for event rate re-entry protocol development.
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ГОСТ |
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Vallejos J. A., McKinnon S. Omori’s Law Applied to Mining-Induced Seismicity and Re-entry Protocol Development // Pure and Applied Geophysics. 2009. Vol. 167. No. 1-2. pp. 91-106.
ГОСТ со всеми авторами (до 50) Скопировать
Vallejos J. A., McKinnon S. Omori’s Law Applied to Mining-Induced Seismicity and Re-entry Protocol Development // Pure and Applied Geophysics. 2009. Vol. 167. No. 1-2. pp. 91-106.
RIS |
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TY - JOUR
DO - 10.1007/s00024-009-0010-7
UR - https://doi.org/10.1007/s00024-009-0010-7
TI - Omori’s Law Applied to Mining-Induced Seismicity and Re-entry Protocol Development
T2 - Pure and Applied Geophysics
AU - Vallejos, J. A.
AU - McKinnon, S.D
PY - 2009
DA - 2009/12/22
PB - Springer Nature
SP - 91-106
IS - 1-2
VL - 167
SN - 0033-4553
SN - 1420-9136
SN - 0033-4533
ER -
BibTex |
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BibTex (до 50 авторов) Скопировать
@article{2009_Vallejos,
author = {J. A. Vallejos and S.D McKinnon},
title = {Omori’s Law Applied to Mining-Induced Seismicity and Re-entry Protocol Development},
journal = {Pure and Applied Geophysics},
year = {2009},
volume = {167},
publisher = {Springer Nature},
month = {dec},
url = {https://doi.org/10.1007/s00024-009-0010-7},
number = {1-2},
pages = {91--106},
doi = {10.1007/s00024-009-0010-7}
}
MLA
Цитировать
Vallejos, J. A., and S.D McKinnon. “Omori’s Law Applied to Mining-Induced Seismicity and Re-entry Protocol Development.” Pure and Applied Geophysics, vol. 167, no. 1-2, Dec. 2009, pp. 91-106. https://doi.org/10.1007/s00024-009-0010-7.
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