Citation: | WANG BIQUAN, WANG CHUNZHEN. 1983: TEMPORAL AND SPATIAL FEATURES OF AFTERSHOCK SEQUENCES. Acta Seismologica Sinica, 5(4): 383-396. |
[1] H. Benioff, Earthquakes and rock creep,B. S. S. A., 41, 1, 35——69, 1951.
[2] 茂木清夫,On the time distribution of after shocks accompanying the recent major earthquakes in and near Japan,B.R. R. L, 40, 107——124, 1962 [3] T. Utau, Aftershocks and earthquake statistics (IV), Journal of Faculty of Science, Hokkaido Univ., IV, 1, 1972. [4] V. Cagnetti and V. Pasquale, The earthquake Sequence in Friuli, Italy, 1976, B. S. S. d., 69, 6,1797——1818, 1979. [5] L. Knopoff, Model for aftershock occurrence, Geophysical Monograph Series, 16, Flow and Fracture of Rocks, 1972. [6] B. T. Brady, Theory of earthquakes II. inclusion tlieory of erustal earthquakes, Pure Appli. Geophy., 113,1——2, 149——168, 1975. [7] C. H. Scholz, Microfracturing and the inelastic of rock in compression, Jour. Geophy. Resea. 1417——1432. 1968. [8] 吴开统等,海城地震序列的特征,地球物理学报,19, 2, 95——109, 1976. [9] 刘正荣等,1974年5月11日云南省永善一大关地震,地球物理学报,20, 2, 110——114,1977. [10] 蜀水,炉霍7.9级地震特征和该区的地震活动性,地球物理学报,17, 2, 77——83, 1974. [11] 陈立德等,1976年龙陵地震,地震出版社,1979. [12] 王碧泉等,强余震的准周期性,地震学报,1, 2, 154——165,1979. [13] 谷继成等,强余震的时间分布特征及其理论解释,地球物理学报,22, 1, 32 —— 46, 1979. [14] 魏柏林,余震震源机制变化的原因,地球物理学报,23, 1, 25——34, 1980, [15] 傅征祥,1978年5月18日海城6级地震前地震活动的某些特征,地震学报,3, 2, 118——125, 1981.
[1] H. Benioff, Earthquakes and rock creep,B. S. S. A., 41, 1, 35——69, 1951.
[2] 茂木清夫,On the time distribution of after shocks accompanying the recent major earthquakes in and near Japan,B.R. R. L, 40, 107——124, 1962 [3] T. Utau, Aftershocks and earthquake statistics (IV), Journal of Faculty of Science, Hokkaido Univ., IV, 1, 1972. [4] V. Cagnetti and V. Pasquale, The earthquake Sequence in Friuli, Italy, 1976, B. S. S. d., 69, 6,1797——1818, 1979. [5] L. Knopoff, Model for aftershock occurrence, Geophysical Monograph Series, 16, Flow and Fracture of Rocks, 1972. [6] B. T. Brady, Theory of earthquakes II. inclusion tlieory of erustal earthquakes, Pure Appli. Geophy., 113,1——2, 149——168, 1975. [7] C. H. Scholz, Microfracturing and the inelastic of rock in compression, Jour. Geophy. Resea. 1417——1432. 1968. [8] 吴开统等,海城地震序列的特征,地球物理学报,19, 2, 95——109, 1976. [9] 刘正荣等,1974年5月11日云南省永善一大关地震,地球物理学报,20, 2, 110——114,1977. [10] 蜀水,炉霍7.9级地震特征和该区的地震活动性,地球物理学报,17, 2, 77——83, 1974. [11] 陈立德等,1976年龙陵地震,地震出版社,1979. [12] 王碧泉等,强余震的准周期性,地震学报,1, 2, 154——165,1979. [13] 谷继成等,强余震的时间分布特征及其理论解释,地球物理学报,22, 1, 32 —— 46, 1979. [14] 魏柏林,余震震源机制变化的原因,地球物理学报,23, 1, 25——34, 1980, [15] 傅征祥,1978年5月18日海城6级地震前地震活动的某些特征,地震学报,3, 2, 118——125, 1981. |