Citation: | 1986: THE DEVELOPMENT OF b-VALUE SIMULATED EXPERIMENTS AND THE BEGINING OF b-VALUE SIMULATED EXPERIMENTS IN CHINA. Acta Seismologica Sinica, 8(3): 330-333. |
[1] 石本已四雄,飯田汲事,微動計にょろ地震戮侧(1),地震研究所彙報,17, 443——478, 1939.
[2] Gutenberg, B., and C. F. Richter, Seismicity of the Earth, Geol. Soc. Am., Spec. Papers, No. 34,131, 1941. [3] Suyehiro, S., T. Asada, and M. Ohtake., Foreshocks and aftershocks accompanying a perceptible earthquake in central Japan, Pap. Met. Geophys, 15, 71——88, 196——1. [4] 神村三郎,石本·飯田の统機式と割れ目现象,地震,2, 88——83, 1955, [5] Vinogradov, S. D., On the distribution of the number of fractures independence on the energy 1i——berated by the destruction of rocks, Bull. Acad. Soc. USSR. Geophys. Ser, 1292——1293, 1959. [6] Mogi, K., Study of elastic shocks caused by the fracture of heterogeneous materials and its raIations to earthquake phenomena, Bull. Earthq. Res. Inst, 40, 125——173, 1962. [7] Mogi, K., Magnitude——frequency relation for elastic shocks acmmhanying fracture of various materi——aIs and some related problems in earthquakes (2), Bull. Earthq. Res. Inst, 40, 831——853, 1962. [8] Scholz, C. H., The frequency——magnitude relation of microfracturing in rock and its relation to ear——thquakes, Bull. Seismol. Soc. Am, 58, 399——115, 1968. [9] 茂木清夫,地震一その本性をそぐろ,東京大学出版会,1981. [10] 平田隆幸,柳谷俊,寺田孚,大岛花岗岩にぉけろクリーフ゜時の凳生時系列につムて,地震,,38, 159——172, 1985, [11] Atkinson, B. K., and R D. Rawlings, Acoustic emission during stress corrosion cracking in rocks,in: Earthquake Prediction, An International Review, Maurice Ewing Series 4, 605——616, 1984.
[1] 石本已四雄,飯田汲事,微動計にょろ地震戮侧(1),地震研究所彙報,17, 443——478, 1939.
[2] Gutenberg, B., and C. F. Richter, Seismicity of the Earth, Geol. Soc. Am., Spec. Papers, No. 34,131, 1941. [3] Suyehiro, S., T. Asada, and M. Ohtake., Foreshocks and aftershocks accompanying a perceptible earthquake in central Japan, Pap. Met. Geophys, 15, 71——88, 196——1. [4] 神村三郎,石本·飯田の统機式と割れ目现象,地震,2, 88——83, 1955, [5] Vinogradov, S. D., On the distribution of the number of fractures independence on the energy 1i——berated by the destruction of rocks, Bull. Acad. Soc. USSR. Geophys. Ser, 1292——1293, 1959. [6] Mogi, K., Study of elastic shocks caused by the fracture of heterogeneous materials and its raIations to earthquake phenomena, Bull. Earthq. Res. Inst, 40, 125——173, 1962. [7] Mogi, K., Magnitude——frequency relation for elastic shocks acmmhanying fracture of various materi——aIs and some related problems in earthquakes (2), Bull. Earthq. Res. Inst, 40, 831——853, 1962. [8] Scholz, C. H., The frequency——magnitude relation of microfracturing in rock and its relation to ear——thquakes, Bull. Seismol. Soc. Am, 58, 399——115, 1968. [9] 茂木清夫,地震一その本性をそぐろ,東京大学出版会,1981. [10] 平田隆幸,柳谷俊,寺田孚,大岛花岗岩にぉけろクリーフ゜時の凳生時系列につムて,地震,,38, 159——172, 1985, [11] Atkinson, B. K., and R D. Rawlings, Acoustic emission during stress corrosion cracking in rocks,in: Earthquake Prediction, An International Review, Maurice Ewing Series 4, 605——616, 1984. |