| Citation: |
P. F. CHEN, P. C. W. FUNG . 1988: A NUMERICAL STUDY OF SOME HORIZONTAL SOURCE FIELD EFFECTS ON THE TRANSFER FUNCTIONS AND THE AMPLITUDE RATIOS IN GEOMAGNETIC INDUCTION INVESTIGATION. Acta Seismologica Sinica, 10(2): 192-205.
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[1] Bcamish, D., A geomagnetic precursor to the 1979 Carlisle earthquake, Geophys. J. R, astr. Soc.. 1982, 68,531——543.
[2] Honkura, Y. and S. Koyama, Observations of shortperiod geomagnetic variations at Nakaizu (1), Bull. Earthq. Rrr. Inst., Univ, Tokyo, 1978, 53, 925——930. [3] Honkura, Y., Current research in earthquake prediction I, edited by T. Rikitake, 352——354, 1981, Center for Academic I'ublicatinns Japan, Tokyo [4] witt——Taylor, C, R. and J. T. Weaver, On the finite difference solution of two——dimensional induction problems, Geophys. J. R. artr. Sac., 1976, 47, 375——396. [5] Chen, P. F., On the finite difference metliod of threedimensional electromagnetic induction problem, Aila Ccaphysica Sinica, 1985, 28, 268——281. [6] Zhdanov, M. S,N. G. Golubev, V.V. Spichak, and 1v. M. Varentsov, The construction of effective methods for electromagnetic modelling, Geophyr. J. R. aszr. Soc., 1982, 68, 589——607 [7] Weaver, J. T. and C. R. Brewitt——Taylor, Improved boundary conditions for the numerical solution of E——po——larization problems in geomagnetic induction, Geaphys. J. R. aszr. Sac., 1978, 54, 309——317. [8] Gough, D. L, F, E. M. Lilley and M. W. McElhinny, A polarization——sensitive magnetic variation anomaly in South Australia, Nature, 1972, 239, 88——91. [9] Jones, F. W., The perturbation of linearly and circularly polarized geomagnetic fields by a non——symmetric twoisland structure at three periods, J. Geomag. Geoelecar., 1974, 26, 295——310. [10] Rokityansky, I, L, Geoelectromagnetic Investigation of the Earth's Crust and Mantle, 381, 1982, Springer—— Verlag, Berlin. [11] Parkinson, W. D. and B. A. Hobbs, Conditions for the geomagnetic induction relatinnsliip, Phys. Earth Ylanra Intrr., 1979, 19, 5——6. [12] Lilley, F. E. M. and D. J, Bennett, Linear relationship in geomagnetic variation studies, Phys. Earth Planet Into., 197.1, 7, 9——14. [13] Frazer, R. A., W, J. Duncan and A. R. Collar, Elementary Matrices, 1947, Cambridge University Press,London,Parkinson, W. D., Directions of rapid geomagnetic fluctuations. ueophys. J. R. astr. Soc., 1959, 2, 1——14. [14] Reddy, I. K., D. Rankin and R. J. Phillips, Three——dimensional modelling in magnetotalluric and magnetic variational sounding, Geophys. J. R. astr. Sac., 1977, S1, 313——325. [15] IIiblis, R. D. and F. W. Jones, The calculation of perturhation and induction arrows for a three——dimensional conductivity model, J. Cconaag, Ceoelecar., 1976, 28, 283——293. [16] Chen, P. F. and 1'. C, W. Fung, Significance of the sign changing of the imaginary arrows in geomagnetic induction investigation, Gcophys. J. R, astr. Soc., 1985, 80, 257——263.
[1] Bcamish, D., A geomagnetic precursor to the 1979 Carlisle earthquake, Geophys. J. R, astr. Soc.. 1982, 68,531——543.
[2] Honkura, Y. and S. Koyama, Observations of shortperiod geomagnetic variations at Nakaizu (1), Bull. Earthq. Rrr. Inst., Univ, Tokyo, 1978, 53, 925——930. [3] Honkura, Y., Current research in earthquake prediction I, edited by T. Rikitake, 352——354, 1981, Center for Academic I'ublicatinns Japan, Tokyo [4] witt——Taylor, C, R. and J. T. Weaver, On the finite difference solution of two——dimensional induction problems, Geophys. J. R. artr. Sac., 1976, 47, 375——396. [5] Chen, P. F., On the finite difference metliod of threedimensional electromagnetic induction problem, Aila Ccaphysica Sinica, 1985, 28, 268——281. [6] Zhdanov, M. S,N. G. Golubev, V.V. Spichak, and 1v. M. Varentsov, The construction of effective methods for electromagnetic modelling, Geophyr. J. R. aszr. Soc., 1982, 68, 589——607 [7] Weaver, J. T. and C. R. Brewitt——Taylor, Improved boundary conditions for the numerical solution of E——po——larization problems in geomagnetic induction, Geaphys. J. R. aszr. Sac., 1978, 54, 309——317. [8] Gough, D. L, F, E. M. Lilley and M. W. McElhinny, A polarization——sensitive magnetic variation anomaly in South Australia, Nature, 1972, 239, 88——91. [9] Jones, F. W., The perturbation of linearly and circularly polarized geomagnetic fields by a non——symmetric twoisland structure at three periods, J. Geomag. Geoelecar., 1974, 26, 295——310. [10] Rokityansky, I, L, Geoelectromagnetic Investigation of the Earth's Crust and Mantle, 381, 1982, Springer—— Verlag, Berlin. [11] Parkinson, W. D. and B. A. Hobbs, Conditions for the geomagnetic induction relatinnsliip, Phys. Earth Ylanra Intrr., 1979, 19, 5——6. [12] Lilley, F. E. M. and D. J, Bennett, Linear relationship in geomagnetic variation studies, Phys. Earth Planet Into., 197.1, 7, 9——14. [13] Frazer, R. A., W, J. Duncan and A. R. Collar, Elementary Matrices, 1947, Cambridge University Press,London,Parkinson, W. D., Directions of rapid geomagnetic fluctuations. ueophys. J. R. astr. Soc., 1959, 2, 1——14. [14] Reddy, I. K., D. Rankin and R. J. Phillips, Three——dimensional modelling in magnetotalluric and magnetic variational sounding, Geophys. J. R. astr. Sac., 1977, S1, 313——325. [15] IIiblis, R. D. and F. W. Jones, The calculation of perturhation and induction arrows for a three——dimensional conductivity model, J. Cconaag, Ceoelecar., 1976, 28, 283——293. [16] Chen, P. F. and 1'. C, W. Fung, Significance of the sign changing of the imaginary arrows in geomagnetic induction investigation, Gcophys. J. R, astr. Soc., 1985, 80, 257——263. |
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