| Citation: |
GAO LONGSHENGup, LI SONGLINup2com . 1985: THE EXPERIMENTAL RESULTS OF VARIATIONS IN THE SUSCEPTIBILITY OF ROCK SAMPLES UNDER UNIAXIAL STRESS BY TWO DIFFERENT APPROACHES. Acta Seismologica Sinica, 7(3): 285-299.
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[1] Nagata, T., Tectonomagnetism, IAGA Bulletin, No`. 27, 12——42, Madrid, Spain, 1969.
[2] Lapma, IvI. Yi., Geomagnetism and seismological phenomena, Izv. Akad. Nauk. USSR Fix. Zemli,No. 5, 1, 1953. [3] Kean, W. F., R. Day, M. Fuller, and V. A. Schmidt, The effect of uniaxial compression on the initial Susceptibility of rocks as a function of grain size and composition of their constituent titanomagnetites, J. Geophys. Res., 81, 861——872, 1976. [4] Martin III, R. J., R. E. Habermann, and M. Wyss, The effect of stresses cycling and inelastic volumettic strain on remanent magnetization, J. Geophy. Rc"r,84, 3485——3496, 1978. [5] 祁贵仲,“膨胀”磁效应,地球物理学报,21, 18——33,1978, [6] 徐世浙、关于压磁效应和膨胀磁效应,地震学报,1, 81——89,1979. [7] Rikitake, T., Geomagnetism and earthquake prediction, Tectonophysics, 6, 59——68, 1968 [8] Smith, B. E. and M. J. 5. Johnston, A tectonomagnetic effect observed before a magnitude 5.2 earthquake near HoIlister, California,J.Geophys. Res., 81, 3556——3560, 1976. [9] 范国华、侯作中、詹志佳、黄平章,唐山地震对北京地区地磁场总强度的影响,地震学报,1, 1,39——49, 1979. [10] Kalashnikov, A. G. and S. P. Kapitsa, Magnetic susceptibility of volcanic rocks under elastic streses, Dokl. Akad. Nauk USSR, 86, 521, 1952. [11] Kapitsa, S. P., Magnetic properties of eruptive rocks exposed to mechanical stresses, Izv. Akad.Nauk USSR Fiz. Zemli, No, 6, 489, 1955. [12] Nagata, T., Magnetic susptibiIity of compressed rocks,].Geomag. Geoelectr., 18, 73——80, 1966. [13] Ohnaka, M., and H. Kinoshita, Effect of axial stress upon initial susceptibility,J.Geomag. Geoelectr., 20, 107——109, 1968. [14] Stacey, F. D., Theory of magnetic susceptibility of stressed rocks Phil. Mag., 7, 551——556, 1962. [15] 北京大学物理系《铁磁学》编写组编,铁磁学131——133,科学出版社,1,,6, [16] Na,ata, T., Basic magnetic properties of rocks under the effects of mechanical stresses, Tectonophysics, 9, 167——195, 1970. [17] Nersesov, I. L., A. N. Semionov, and I. G. 5imbireva, Space time distribution of ratios of traveltimes of transverse and Longitudinal wares in Garm region, Exp. Seismology, Sbornik, 334, 1971. [18] Johnston, A. C., Max Wyss and R. E. Habetmann, Robert koyanagi, Stability and change of p——wave, travel times in the crust (abstract), EOS, 62, 964, 1981. [19] hijachkin, V. L, W. F.Brace G. A. SoboIev, and J. H. Dieterich, Two models for earthquake forerunners, Pageoph, 113 169——181. 1975. [20] Mizutani, H. and T. Ishido, A new interpretation of magnetic field variation associated with the Matsushito earthquakes, j. Geomag. Geoelectr., 28 179——188 1976.
[1] Nagata, T., Tectonomagnetism, IAGA Bulletin, No`. 27, 12——42, Madrid, Spain, 1969.
[2] Lapma, IvI. Yi., Geomagnetism and seismological phenomena, Izv. Akad. Nauk. USSR Fix. Zemli,No. 5, 1, 1953. [3] Kean, W. F., R. Day, M. Fuller, and V. A. Schmidt, The effect of uniaxial compression on the initial Susceptibility of rocks as a function of grain size and composition of their constituent titanomagnetites, J. Geophys. Res., 81, 861——872, 1976. [4] Martin III, R. J., R. E. Habermann, and M. Wyss, The effect of stresses cycling and inelastic volumettic strain on remanent magnetization, J. Geophy. Rc"r,84, 3485——3496, 1978. [5] 祁贵仲,“膨胀”磁效应,地球物理学报,21, 18——33,1978, [6] 徐世浙、关于压磁效应和膨胀磁效应,地震学报,1, 81——89,1979. [7] Rikitake, T., Geomagnetism and earthquake prediction, Tectonophysics, 6, 59——68, 1968 [8] Smith, B. E. and M. J. 5. Johnston, A tectonomagnetic effect observed before a magnitude 5.2 earthquake near HoIlister, California,J.Geophys. Res., 81, 3556——3560, 1976. [9] 范国华、侯作中、詹志佳、黄平章,唐山地震对北京地区地磁场总强度的影响,地震学报,1, 1,39——49, 1979. [10] Kalashnikov, A. G. and S. P. Kapitsa, Magnetic susceptibility of volcanic rocks under elastic streses, Dokl. Akad. Nauk USSR, 86, 521, 1952. [11] Kapitsa, S. P., Magnetic properties of eruptive rocks exposed to mechanical stresses, Izv. Akad.Nauk USSR Fiz. Zemli, No, 6, 489, 1955. [12] Nagata, T., Magnetic susptibiIity of compressed rocks,].Geomag. Geoelectr., 18, 73——80, 1966. [13] Ohnaka, M., and H. Kinoshita, Effect of axial stress upon initial susceptibility,J.Geomag. Geoelectr., 20, 107——109, 1968. [14] Stacey, F. D., Theory of magnetic susceptibility of stressed rocks Phil. Mag., 7, 551——556, 1962. [15] 北京大学物理系《铁磁学》编写组编,铁磁学131——133,科学出版社,1,,6, [16] Na,ata, T., Basic magnetic properties of rocks under the effects of mechanical stresses, Tectonophysics, 9, 167——195, 1970. [17] Nersesov, I. L., A. N. Semionov, and I. G. 5imbireva, Space time distribution of ratios of traveltimes of transverse and Longitudinal wares in Garm region, Exp. Seismology, Sbornik, 334, 1971. [18] Johnston, A. C., Max Wyss and R. E. Habetmann, Robert koyanagi, Stability and change of p——wave, travel times in the crust (abstract), EOS, 62, 964, 1981. [19] hijachkin, V. L, W. F.Brace G. A. SoboIev, and J. H. Dieterich, Two models for earthquake forerunners, Pageoph, 113 169——181. 1975. [20] Mizutani, H. and T. Ishido, A new interpretation of magnetic field variation associated with the Matsushito earthquakes, j. Geomag. Geoelectr., 28 179——188 1976. |
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