引文
[1]Sellers E J,Klerck P.Modeling of the effect of discontinuities on theextent of the fracture zone surrounding deep tunnels[J].Tunnelingand Underground Space Technology,2000,15(4):463-469.
[2]Malan D F,Spottiswoode S M.Time-dependent fracture zone behav-ior and seismicity surrounding deep level stopping operations[A].Rockburst and Seismicity in Mines[C].Rotterdam:A.A.Balkema,1997:173-l77.
[3]何满潮.深部的概念体系及工程评价指标[J].岩石力学与工程学报,2005,24(16):2 854-2 858.He Manchao.Conception system and evaluation indexes for deep en-gineering[J].Chinese Journal of Rock Mechanics and Engineering,2005,24(16):2 854-2 858.
[4]徐则民,黄润秋,王士天.隧道的埋深划分[J].中国地质灾害与防治学报,2000,11(4):5-10.Xu Zemin,Huang Runqiu,Wang Shitian.Tunnel classifying in lightof depth[J].The Chinese Journal of Geological Hazard and Control,2000,11(4):5-10.
[5]景海河.深部工程围岩特性及其变形破坏机制研究[D].北京:中国矿业大学(北京),2002.Jing Haihe.Research on the characteristics of the rock mass in deepengineering and its deformation mechanism[D].Beijing:ChineseUniversity of Mining and Technology(Beijing),2002.
[6]梁政国.煤矿山深浅部开采界线划分问题[J].辽宁工程技术大学学报(自然科学版),2001,20(4):554-556.Liang Zhengguo.The question about the boundary division of deep ofshallow part’s coal mining[J].Journal of Liaoning Technical Uni-versity(Natural Science),2001,20(4):554-556.
[7]钱七虎.深部岩体工程响应的特征科学现象及“深部”的界定[J].东华理工学院学报,2004,27(1):1-5.Qian Qihu.The characteristic scientific phenomena of engineeringresponse to deep rock mass and the implication of deepness[J].Journal of East China Institute of Technology,2004,27(1):1-5.
[8]李铁.采矿诱发地震机理及其安全对策的研究[D].北京:北京科技大学,2007.Li Tie.Study on the mechanism of mining-induced seismicity and itssafety control[D].Beijing:University of Science&Technology Bei-jing,2007.
[9]Cai M F,Ji H G,Wang J A.Study on the time-space-strength rela-tion for mining seismicity at Laohutai coal mine and its prediction[J].International Journal of Rock Mechanics&Mining Sciences,2005,42(1):145-151.
[10]Benioff H.Earthquakes and rock creep Part 1:Creep characteris-tics of rocks and the origin of afterchocks[J].Bull.Seismol.Soc.America,1951,41(1):31-62.
[11]Bullen Kert Edward,Bolt Bruce A.An introduction to the theory ofseismology[M].New York:Cambridge University Press,1985.
[12]Gutenberg B,Richter C F.Seismicity of the earth and associatedphenomenon[M].Princeton:Princeton University Press,1954.
[13]雷兴林,佐藤隆司,西泽修.花岗岩变形破坏的阶段性模型—应力速度及预存微裂纹密度对断层形成过程的影响[J].地震地质,2004,26(3):436-449.Lei Xinglin,Takashi Satoh,Osamu Nishizawa.Three-stage fractu-ring model for granitic rocks under triaxial compression:role of mi-crocrack density and stress rate on fault formation[J].Seismologyand Geology,2004,26(3):436-449.
[14]陈颙,陈凌.分形几何学[M].北京:地震出版社,2005.Chen Yong,Chen Ling.Fractal geometry[M].Beijing:Seismologi-cal Press,2005.
[15]Gibowicz S J,Kijko A.An introduction to mining seismology[M].San Diego:Academic Press,1994.
[16]陈忠辉,谭国焕,杨文柱.不同围压作用下岩石损伤破坏的数值模拟[J].岩土工程学报,2001,23(5):576-580.Chen Zhonghui,Tan Guohuan,Yang Wenzhu.Numerical simulationof damage and failure of rocks under different confining pressures[J].Chinese Journal of Geotechnical Engineering,2001,23(5):576-580.
[17]李铁,蔡美峰,王金安,等.深部开采冲击地压与瓦斯相关性的探讨[J].煤炭学报,2005,30(5):562-567.Li Tie,Cai Meifeng,Wang Jin’an,et al.Discussion on relativity be-tween rockburst and gas in deep exploitation[J].Journal of ChinaCoal Society,2005,30(5):562-567.