Summary and Considerations about Characteristics of Borehole Stress Meter for Continuous Observation
Author:
Affiliation:
1. Tono Research Institute of Earthquake Science (TRIES), Association for the Development of Earthquake Prediction (ADEP)
Publisher
Seismological Society of Japan
Link
https://www.jstage.jst.go.jp/article/zisin/72/0/72_2018-9/_pdf
Reference11 articles.
1. Aki, K., 1968, Seismic displacements near a fault, J. Geophys. Res., 73, 5359-5376, doi:10.1029/JB073i016p05359.
2. Aki, K. and P. G. Richards, 2002, Quantitative Seismology, 2nd ed., University Science Books, Sausalito, 700pp.
3. Gladwin, M. T., 1984, High-precision multicomponent borehole deformation monitoring, Rev. Sci. Instrum., 55, 2011-2016, 1984, doi:10.1063/1.1137704.
4. Ishii, H. and T. Kato, 1989, Detectabilities of earthquake precursors using GPS, EDM and strain meters, with special reference to the 1923 Kanto earthquake, J. Geod. Soc. Japan, 35, 75-83, doi:10.11366/sokuchi1954.35.75.
5. Ishii, H., T. Yamauchi, S. Matsumoto, Y. Hirata, and S. Nakao, 2002, Development of multi-component borehole instrument for earthquake prediction study: some observed example of precursory and co-seismic phenomena relating to earthquake swarms and application of the instrument for rock mechanics, Seismogenic Process Monitoring, Balkema, The Netherlands, 365-377.
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