b值模拟实验的进展和我国b值模拟实验的开端
THE DEVELOPMENT OF b-VALUE SIMULATED EXPERIMENTS AND THE BEGINING OF b-VALUE SIMULATED EXPERIMENTS IN CHINA
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摘要: 本文简要地回顾了国外地震学家在b值模拟实验方面所做的工作和主要观点.叙述了1985年下半年国家地震局的三个研究单位六个研究组在b值模拟实验中得到的主要结果.Abstract: Abrief review on work and viewpoint of foreign seismologists about b-value simulated experiments was made. The major results obtained by six study groups of three institutes of SSBin b-value simulated experiments in second half of 1985 were described.
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[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.
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