| Citation: |
LUCILE M. JONESup, WANG BIQUANup2, XU SHAOXIEup2, THOMAS J. FITCHup3loans.com sh advlucashadv. 1983: THE FORESHOCK SEQUENCE OF THE FEBRUARY, 4,1975,HAICHENG EARTHQUAKE (M=7.3). Acta Seismologica Sinica, 5(1): 1-14.
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[1] H. Mogi, Some discussions on aftershocks, foreshocks, and earthquake swarli}:The fracture of a semi——infinite caused by an inner stress origin and its relation to earthquake phenomena 3, Bull.Earthquake yes. Inat. Tokyo an%v., 41, 815——658, 1963.
[2] L. M. Jones, and P. Molnar, Some characteristics of foreshocks and their possible relationship to earthquake prediction and premonitory slip on faults, J. Geophys. Rea., 84, 359E——3608, 1979. [3] Y. Kagan, and L. linopoff, Statistical atndy of the occurrence of shallow earthqxxakes, Geophys.J. R. dstron. Soc., 55, 67——86, 1878. [4] E. R. Engdahl, and C. giaslinger, Seismological preaursars to—— a magnitude 5 earthquake in the Central Aleutian Islands, J,Phys,Earth, 25, s243——a250, 1977. [5] A. Lindh, G. Fuis, and C. Mantis, Seismic amplitude measurements suggest foreehoeke have different focal mechanisms than aftershocks, Science, 201, 56——59, 1978. [6] S. Billington, E.R.Engdahl, and 8. Price, Changes in the seismieitp and focal mechanism of ——small earthquakes prior to an Ma=6.7 earthquake in the Central Aleutian Island Arc, Earrthquake Prediction, An International Review, Maxirice Ewing 8er. 3, 4, edited by D. W. Simpson and—— P. G. Richards, pp. 348——356, AGU, Washington, D. C., 1981. [7] J. Cigar, Source processes of the Haicheng, China eartahquake from observations of P and S waves,Bull. Seiamod. Soc. dm., 69, 1903——1916, 1979. [8] 吴开统、岳明生等,海城地晨序列的特征,地球物理学报,19, 2, 95——109, 1976, [9] T. Fitch. and H. J. Muirhead, Depths to larger earthquakes associated with crustal loading, Geophya. J. R. datron. Soc., 37, 285——296, 1974. [10] J. Jackeon, ands T. Fitch, 8eismoteetonic implications of relocated aftershock sequences in Iran and Turkey: an application of the master event technique, Geaphys. J. R. datron. .Soc., 57, 209——229, 1979. [11] T. Fitch, and J. M. W. Ryan, Inversion for Vr/Y, in shallow source regions, Geophys. J. R. dstron. Soc., 44, 253——267, 1976. [12] 金严、赵毅等,辽宁省海城地晨前晨震源错动方式的一个特点,地球物理学报,19, 3, 156——164,1976, [13] L. M. Jones, Q. Deng, and P. Jiang, The role of conjugate faults in the development and oceurrence of earthquakes (in Chinese), Seiamiol. Geol., 2, 19——26, 1980. [14] B. A. Bolt, J. Btifler, and R. Urhammer, The Briones Hills earthquake swarm of January 8, 1977. Contra Costa County, California, Bull. Se%smol. Soc. dm., 67, 1555——1564, 1977. [15] 陈顺,用震源机制一致性作为描述地晨活动性的新参数,地球物理学报,21, 2, 142——159, 1978, [16] A. Ben——Menahem, S.W.Smith and T. L. Teng, A procedure for s.'ource studies from. spectrums of long——period seismic body waves, Bull. Seismol. Soc, dm., 55, 203——235, 1965. [17] 顾浩鼎、陈运泰等,197,年2月4日辽宁省海城地晨的震源机制,地球物理学报,19, 4, 270——285,1976. [18] P. Paria, and G. Sih, 8tresa analysis of cracks, Symposium on Fracture Toughm,ess Testvng and Applications, ASTM, Spea. Teoh. Publ., 381, 30——81, 1965. [19] Q. Deng, P. Jiang, L. Jones, and P. Molnar, A preliminary analysis of reported changes in ground water and anomalous animal behavior befoxe the 4 February 1975 Haicheng earthquake, Earth——quake Prediction, An International Review, Mancrice Ewing Ser. 3, 4, edited by D.W. Simgaon and P. G. Richarda, pg. 543——565, AGU, Washington, D. C., g. 543——565, 1981. [20] C. B. Raleigh, et al., Prediction of the Haicheng earthquake, Eos. Trans. AGU, 58, 236——272, 1977. [21] H. ganamori, and D. Anderson, Theoretical basis of some empirical relations in seismology, Bull. Seism.ol. Soc. din,65, 1073——109:5 1975.
[1] H. Mogi, Some discussions on aftershocks, foreshocks, and earthquake swarli}:The fracture of a semi——infinite caused by an inner stress origin and its relation to earthquake phenomena 3, Bull.Earthquake yes. Inat. Tokyo an%v., 41, 815——658, 1963.
[2] L. M. Jones, and P. Molnar, Some characteristics of foreshocks and their possible relationship to earthquake prediction and premonitory slip on faults, J. Geophys. Rea., 84, 359E——3608, 1979. [3] Y. Kagan, and L. linopoff, Statistical atndy of the occurrence of shallow earthqxxakes, Geophys.J. R. dstron. Soc., 55, 67——86, 1878. [4] E. R. Engdahl, and C. giaslinger, Seismological preaursars to—— a magnitude 5 earthquake in the Central Aleutian Islands, J,Phys,Earth, 25, s243——a250, 1977. [5] A. Lindh, G. Fuis, and C. Mantis, Seismic amplitude measurements suggest foreehoeke have different focal mechanisms than aftershocks, Science, 201, 56——59, 1978. [6] S. Billington, E.R.Engdahl, and 8. Price, Changes in the seismieitp and focal mechanism of ——small earthquakes prior to an Ma=6.7 earthquake in the Central Aleutian Island Arc, Earrthquake Prediction, An International Review, Maxirice Ewing 8er. 3, 4, edited by D. W. Simpson and—— P. G. Richards, pp. 348——356, AGU, Washington, D. C., 1981. [7] J. Cigar, Source processes of the Haicheng, China eartahquake from observations of P and S waves,Bull. Seiamod. Soc. dm., 69, 1903——1916, 1979. [8] 吴开统、岳明生等,海城地晨序列的特征,地球物理学报,19, 2, 95——109, 1976, [9] T. Fitch. and H. J. Muirhead, Depths to larger earthquakes associated with crustal loading, Geophya. J. R. datron. Soc., 37, 285——296, 1974. [10] J. Jackeon, ands T. Fitch, 8eismoteetonic implications of relocated aftershock sequences in Iran and Turkey: an application of the master event technique, Geaphys. J. R. datron. .Soc., 57, 209——229, 1979. [11] T. Fitch, and J. M. W. Ryan, Inversion for Vr/Y, in shallow source regions, Geophys. J. R. dstron. Soc., 44, 253——267, 1976. [12] 金严、赵毅等,辽宁省海城地晨前晨震源错动方式的一个特点,地球物理学报,19, 3, 156——164,1976, [13] L. M. Jones, Q. Deng, and P. Jiang, The role of conjugate faults in the development and oceurrence of earthquakes (in Chinese), Seiamiol. Geol., 2, 19——26, 1980. [14] B. A. Bolt, J. Btifler, and R. Urhammer, The Briones Hills earthquake swarm of January 8, 1977. Contra Costa County, California, Bull. Se%smol. Soc. dm., 67, 1555——1564, 1977. [15] 陈顺,用震源机制一致性作为描述地晨活动性的新参数,地球物理学报,21, 2, 142——159, 1978, [16] A. Ben——Menahem, S.W.Smith and T. L. Teng, A procedure for s.'ource studies from. spectrums of long——period seismic body waves, Bull. Seismol. Soc, dm., 55, 203——235, 1965. [17] 顾浩鼎、陈运泰等,197,年2月4日辽宁省海城地晨的震源机制,地球物理学报,19, 4, 270——285,1976. [18] P. Paria, and G. Sih, 8tresa analysis of cracks, Symposium on Fracture Toughm,ess Testvng and Applications, ASTM, Spea. Teoh. Publ., 381, 30——81, 1965. [19] Q. Deng, P. Jiang, L. Jones, and P. Molnar, A preliminary analysis of reported changes in ground water and anomalous animal behavior befoxe the 4 February 1975 Haicheng earthquake, Earth——quake Prediction, An International Review, Mancrice Ewing Ser. 3, 4, edited by D.W. Simgaon and P. G. Richarda, pg. 543——565, AGU, Washington, D. C., g. 543——565, 1981. [20] C. B. Raleigh, et al., Prediction of the Haicheng earthquake, Eos. Trans. AGU, 58, 236——272, 1977. [21] H. ganamori, and D. Anderson, Theoretical basis of some empirical relations in seismology, Bull. Seism.ol. Soc. din,65, 1073——109:5 1975. |
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