Citation: | F. D. Stacey. 1984: EARTHQUAKE PREDICTION RESEARCH--A PERSONAL VIEW OF THE PROBLEMS AND THE DIRECTIONS WHICH FUTURE WORK SHOULD TAKE. Acta Seismologica Sinica, 6(1): 1-7. |
[1] J. N. Bruise, Implications of earthquake triggering and rupture propagation for eartliquak,prediction based on premonitory phenomena. J. Geophys. Res., 84, 2195——2198, 1979.
[2] Jinqi Hao, L. M. Haatie and F. D. BZtacey, Theory of the aeisrnomagnetic effect: a reaases——ament, Phys. Lett Planet. Int., 28, 129——140, 1982. [3] P. M. Davia, D. D. Jackson, C. A. Searle and R. L. MacPherson. Detection of tectonoma.gne——tic events using multichannel predictive filtering, .7. Geophys. Res., 86, 1731——1737, 1981. [4] I. L. Nersesov, A. N. Semenov and I. G. Himb6a"eva, Space——time distribution oP travel times of transverse and longitudinal waves in the Garm region, In M. A. Sadovsky Exveri——rnrrrtal Seismology, Moscow. Science Publishing House, 334, 1969. [5] D. A. Lockner and J. D. Byerlee, Yeloeity anomalies: an alternative explanation based on laboratory experiments, Pare and Appl. GeoPhys., 116, 765——772, 1978. [6] S. Crampin, Seismic wav a propagation through a cracked solid:polarization as a possible dilatancy diagnostic, Geophys. J. R. Astron. Soc., 53, 467——496, 1978. [7] S. Crampizr, R. Evana, B. User,M.Doyle, J. P. Davie, G. Y. Yegorkina and A. Miller, Obaer——vations of dilato——rncy——induced polarization anomalies land earthquake prediction, Nature, 286,874——877, 1980. [8] I. S. Sacks and D. W. Everteon, A aenetive borehole strain——rate meter, Uarnegie Institution Washington Year Rook 68. 448——452. 1970.
[1] J. N. Bruise, Implications of earthquake triggering and rupture propagation for eartliquak,prediction based on premonitory phenomena. J. Geophys. Res., 84, 2195——2198, 1979.
[2] Jinqi Hao, L. M. Haatie and F. D. BZtacey, Theory of the aeisrnomagnetic effect: a reaases——ament, Phys. Lett Planet. Int., 28, 129——140, 1982. [3] P. M. Davia, D. D. Jackson, C. A. Searle and R. L. MacPherson. Detection of tectonoma.gne——tic events using multichannel predictive filtering, .7. Geophys. Res., 86, 1731——1737, 1981. [4] I. L. Nersesov, A. N. Semenov and I. G. Himb6a"eva, Space——time distribution oP travel times of transverse and longitudinal waves in the Garm region, In M. A. Sadovsky Exveri——rnrrrtal Seismology, Moscow. Science Publishing House, 334, 1969. [5] D. A. Lockner and J. D. Byerlee, Yeloeity anomalies: an alternative explanation based on laboratory experiments, Pare and Appl. GeoPhys., 116, 765——772, 1978. [6] S. Crampin, Seismic wav a propagation through a cracked solid:polarization as a possible dilatancy diagnostic, Geophys. J. R. Astron. Soc., 53, 467——496, 1978. [7] S. Crampizr, R. Evana, B. User,M.Doyle, J. P. Davie, G. Y. Yegorkina and A. Miller, Obaer——vations of dilato——rncy——induced polarization anomalies land earthquake prediction, Nature, 286,874——877, 1980. [8] I. S. Sacks and D. W. Everteon, A aenetive borehole strain——rate meter, Uarnegie Institution Washington Year Rook 68. 448——452. 1970. |