Citation: | ZHU CHUAN-ZHEN, FU CHANG-HONG, LUO SHENG-LIcom sh adv. 1981: STUDY OF EARTHQUAKE SWARMS IN RELATION TO LARGE EARTHQUAKES (NORTH CHINA AREA). Acta Seismologica Sinica, 3(2): 105-117. |
[1] 関谷溥,群凳性地震と地震予知,地震予知研究ッンポジワム,1972
[2] 茂木清夫,地震活动と地震予知,地震予知ッンポジワム,1977 [3] M .Isliida, and H. Kanamori., The foresliock activity of the 1971 san fernaudo earthquake California, BSSA,68, 5,1265——1280,1978 [4] F. F. Evison, Precursory seismi;e sequences in mew Zealand,NZ Jour of Geology and Geo——physics,20,11129——141,1977. [5] F. F. Evison, The precursory earthquake swarm, Phaysics of the earth and Planatary Interiors,15,19——23,1977 [6] 华北地区ML地震目录(1952——1974)地震出版社(待发表). [7] 北京及邻区地震目录汇编,地震出版社(待发表). [8] 张祖胜,唐山7.8级地震的地面形变,欧洲地震委员会地球物理年会报告,1978,斯特拉斯堡. [9] 赛克斯,缓慢地震与应力重新分布,国外地震,3, 10——13, 1979 [10] 许忠淮等,京津唐张地区地震应力场的方向特征,地震学报,1, 2, 121——132, 1979 [11] 约翰逊,粘滑源参数和地震源参数,国外地震,4, 41——43, 1975 [12] T .Mikumo, Source process of deep and Intermediate eartliauakes as inferred from long——period P and S waveforms, Physics of the Earth, 19. 4. 303——320. 1971, [13] 朱传镇等,海城地震前后微震震源参数和介质品质因子,地球物理学报,20, 3, 228——231, 1977. [14] R. Green, A. McGarr, A comparison of the focal mechanism and aftersliock distribution of the Ceres South Africa earthquake of September 29, 1969, BSS9, 62, 3, 869——871, 1972 [15] 张之立等,唐山地震的破裂过程及其力学分析,地震学报,2,2,111——129.1980 [16] 邢台地震总结,地震出版社(待发表). [17] 顾浩鼎等,1975, 2, 4.辽宁省海城地震的震源机制,地球物理学报,19, 4, 270——284, 1976. [18] 吴开统等,海城地震序列的特征,地球物理学报,19, 2, 95——109, 1976. [19] D. F'. Hill, A model of earthquake swarm J. G.R.82. 8. 1347——1352. 1977.
[1] 関谷溥,群凳性地震と地震予知,地震予知研究ッンポジワム,1972
[2] 茂木清夫,地震活动と地震予知,地震予知ッンポジワム,1977 [3] M .Isliida, and H. Kanamori., The foresliock activity of the 1971 san fernaudo earthquake California, BSSA,68, 5,1265——1280,1978 [4] F. F. Evison, Precursory seismi;e sequences in mew Zealand,NZ Jour of Geology and Geo——physics,20,11129——141,1977. [5] F. F. Evison, The precursory earthquake swarm, Phaysics of the earth and Planatary Interiors,15,19——23,1977 [6] 华北地区ML地震目录(1952——1974)地震出版社(待发表). [7] 北京及邻区地震目录汇编,地震出版社(待发表). [8] 张祖胜,唐山7.8级地震的地面形变,欧洲地震委员会地球物理年会报告,1978,斯特拉斯堡. [9] 赛克斯,缓慢地震与应力重新分布,国外地震,3, 10——13, 1979 [10] 许忠淮等,京津唐张地区地震应力场的方向特征,地震学报,1, 2, 121——132, 1979 [11] 约翰逊,粘滑源参数和地震源参数,国外地震,4, 41——43, 1975 [12] T .Mikumo, Source process of deep and Intermediate eartliauakes as inferred from long——period P and S waveforms, Physics of the Earth, 19. 4. 303——320. 1971, [13] 朱传镇等,海城地震前后微震震源参数和介质品质因子,地球物理学报,20, 3, 228——231, 1977. [14] R. Green, A. McGarr, A comparison of the focal mechanism and aftersliock distribution of the Ceres South Africa earthquake of September 29, 1969, BSS9, 62, 3, 869——871, 1972 [15] 张之立等,唐山地震的破裂过程及其力学分析,地震学报,2,2,111——129.1980 [16] 邢台地震总结,地震出版社(待发表). [17] 顾浩鼎等,1975, 2, 4.辽宁省海城地震的震源机制,地球物理学报,19, 4, 270——284, 1976. [18] 吴开统等,海城地震序列的特征,地球物理学报,19, 2, 95——109, 1976. [19] D. F'. Hill, A model of earthquake swarm J. G.R.82. 8. 1347——1352. 1977. |
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