引文
[1]李海波,吴绵拔,龙门石窟文物区岩体波动测试与分析[J]岩土力学,1995, 16(3): 43~48
[2]李建林.三峡工程船闸高边坡岩体宏观力学参数研究[D]重庆建筑大学,1996
[3]张晶瑶.岩体稳定性动态级的声波参数测定与分析[J]煤炭学报. 198611(3):43~50.
[4]梁治安.岩体爆破影响的声波测试[J]岩土力学,1992, 13(4);73~79
[5]赵明阶,徐蓉坝基灌浆效果评价中的波速成像法[J].桂林工学院学报,1996, 16(12):136~142
[6]成都水电设计院.高分辩车工程地震勘探技术研究[R].八五国家科技攻关项目科研报告,1994
[7]吴少武,张绍治运用声波法研究硐体围岩和应力状态[J].地震,1984(6):12~19
[8]王宏图.岩石弹性波理论及其在地应力测试中的应用研究[D].重庆大学,1995
[9]Ridrignes P F. Anistropy of granites. Inter. Congress on Rock mech[M]. Cisbon,1966,721~731.
[10]Douglass P M, Voight B. Anisofropy ofgranites, A reflection of microscopic fabric[J]. Geotechnique, 1969,19(3):376~398.
[11]Thill R E. Velocity anisotropy in dry andsaturated Rock spherres and it elation toRock fabtic[M]. Int. J. Rock Mech.Min. Sci.& Geomech. Abstr, 1973.(10): 535~557.
[12]席道瑛 .砂岩的变形备向异性[J]岩石力学与工程学报,1995,14(1):49~58
[13]Roe R J. Description of crystallite Orientation inpolycrystalline Materials[J].ⅢGeneral Solution ot Ploe Figure Inversion.Journal of Applied bysics, 1965,36(6):2024 ~ 2031.
[14] Roe R J. Inversion of Pole Figures forMsterials Hsving Cubic Crystal symmetry[J] .J. Appl. Phys., 1966, 37 (5).
[15] Sayer C M. Ultrasonic Velocities inanisotropic Polycrystalline aggregate4s [J].J.phys. D., 1982, (15): 2 157~2 167.
[16] Sayer C M. Terture independent determination of residual stress in Polycrystalline aggregates Using Rayleigh Waves[J].J.Phys. D, 1984, (17): L179~L184.
[17] Sayer C M. Angular dependence if gherayleigh wave velocity in Polycrystalline metals with small anisotropy [J], Proc. R.Soc., Lond., 1985, A (40): 175 ~182.
[18] Sayer C M. The influeme of atress on thePrincipal Polarisation direcfions of ultrasonicshear waves in textured stal plates [J]. J.phys., 1984, D (17): 1 399~1 413.
[19] Sayer C M. Inversion of ultrasonic wavevelocity measurements to obtain the microcrack orientaion distribtuion fuxretion in rocks[J]. Ultrasonic, 1988, 26 (3):73 -77.
[20] Sayer C M. Orientation of microcracksforned in rocks during Strain, etlaxation[J]. Int. J. Rock mech. min. Sci.&Geomech. Avstr., 1990, 27 (5): 437-439.
[21] Sayer C M. J G van Munster. Microcrackinduced seismic Amisotropy of sedimeutryrocks [J]. J. G. R. A0, 1991, 96(B10): 16 529~ 16 533.
[22] Sayer C M. Stress-indyeed ultrasonic wavevelocity anisotropy in fractured rock[J].Ultrasonic, 1988, 26 (11): 311 ~317.
[23] Sayr C M. Stress-induced ultrasonicamisotropy in Berea Sandstone [J].Int. J.Rock mech min Sci & Geomech abstr.,1990, 27 (5): 429~436.
[24] Oda M. Similarity of crck geonetry instatislically homogenous rockmiass [J].Mech meteri., 1984, (3): 119~ 129.
[25] Oda M. Pereability tensor for discontinuonsrock masses[J]. Geotcehnique, 1985,35(4): 483~495.
[26] Oda M. A Crack tensor and its relation towave velocity Anisotropy in jointed rockmasses [J].Int. J. Rock mech.min.Sci & Geomech. abstr. 1986, 23(6):387 ~ 397.
[27] Oda M. An experimental study of the elastcity of mylonite rock with random cracks[J]. Int. J. Rock meeh. min. Sci.&Geomech abstr, 1988, 25 (2): 59~69.
[28] Sayer C M. Stress-dependent elastic wavevelocities in shales [J]. Int. J. rockmech. min. Sci & Geomech abstr, 1995,32 (3): 263~267.
[29] Walsh J B. The etlect of cracks on thecomprosibity of rock [J ]. J. G. R.,1965, 70 (20): 381~411.
[30] O'connell R J. Seismic Veloties in dry andSaturated cracked solids[J]. J. G. R.,1974, 79 (35): 5 412~5 425.
[31] Hudson J A. Overall elastic properties of isotropic materials with orbitary distribution ofvircular vracks [J]. Geophy. J. Int.,1990, (102): 465~469.
[32] Kemeny J. Effective moduli non-linear deformation and strength of a cracked elasticsolid[J]. Int. J. Rock meeh. min. Sci.& Geomech. abstr., 1986, (23): 107-118.
[33] Budiansky B, O' connell R J. Elasticmoduli of a cracked solid[J]. Int. J.Solids fructure, 1976, 2 (1); 81~87.
[34] Zimmerman R W. The effect of microcracks on the clastic modali of briffle materials[J]. J. Mater. Sci., Cett. 1985, 26(1 ): 38~ 45.
[35] Hu & Huang. Estimation of the elasticproperties of fractureed rock masses [J].Int. J. Rock mech. Sci.& Geomech.Abstr., 1993, 30 (4):381~394.
[36] Sayer C M, Kachanov M. Asimple technique for finding effective elastic constrants ofcracked solids for argifrary Crack orientationstatistics [J]. Int. J. Solids strudtures,1991, 27 (6): 671~680.
[37] Birch F. The velocity of compressionalwave in rocks to 10 Kilobars [J]. Part I.J. G. R., 1960, 65 (11): 1 083 ~ 1102.
[38] Birch F. the velocity of compressionalwave in rocks to 10 Kilobars [J]. part Ⅱ.J. G. R, 1961, 66 (1): 2 199~2224.
[39] Walsh J B, Brace W F. Elasticity ofrock: A review of some recent theoreticalstudies[J]. Rock mech. Eng. Geol.,1966,(4):283~296.
[40] Walsh J B, Brsce W F . Cracks and poresin rocks Int [J]. cougress on rock mech.,Lisbon, 1966, 641~643.
[41] Simmons G. Velocity of shear waves inRocks to 10 Kilobars [J]. J. G. R.,1964, 69(6): 1 123~1 130.
[42] Singh B. The behavionr of rocks underpressure[ J]. Investigations using ultrasonic. 1960,(201): 719~724.
[43] Nur A. Effects of atress on velocityanisotropy in rocks with cracks[J]. J. G.R., 1971, 76(8): 2 022~2 034
[44]高龙生.中国大陆岩石标本在高压下的弹性波波速研究[J]、地球物理学报,1975,8(1):11~17
[45]蔡忠理.单轴压缩过程中花岗岩的声学特性研究[J]岩土力学, 1986,7(2):27~36
[46] Mao N. Sweeney J, et al. Using a sonictechanique to estimate in situ stresses [J].Rock mechanics in Productivity & Prtec.tion, chapter 18, 1982, 167~175.
[47] Su W H. Peng S S, et al. Derelopmentof ultrasonic methods for measueing in-situtresses at great depth [J]. Min. Sci.&tech., 1983,(1): 21~42
[48]黄承贤,宋大卫.在围压下岩石弹性波速的研究[J].岩土工程学报,1991,13(2): 32~41
[49] Pros Z, Vanek J, et al. The velocity ofelastic wave in Diabase and Greywacke underPressure up to 4 Kilobarus [J]. Studia Geophy. et . Geod., 1962,6(4):347~367.
[50] Winkler K W. Nur A. Seismic attenuationeffects of pore Fluids and Frictional sliding[J]. Geophysics, 1982 47( 1): 1~15.
[51] Johnston D H. Attenuation: Astat-of-the-art symmertry seimic wave attenuation [J].edited by Toksoz M. N. & Johnston D.H., Society of exploration Geophysicists,1981,(2): 123~135
[52] Toksozm M N. Johnston D H, et al. Attenuation of seismic waves in Dry and Saturated rocks: I. Lsboratory Measurements[J]. Geophysics, 1979 44(4): 681~711.
[53] Born W T. Attenuation constatnts of earthmaterials, Geophysics[J]. 1941, 6(1):132~148
[54]陈耕野.单轴压缩下模拟弱面宕石的声波衰减[C]、岩石声学性质论文集东北工学院,1989,32~39.
[55]秦四清.岩石中声波衰减的复合Q模型[J].东北工学院学报, 1991, 12(6):578~582.
[56]易南概.岩石试件声波衰减品质因素Q与全应变过程曲线[C],岩石声学性质论文集,东北工学院, 1989, 10~13.
[57]陈耕野.岩石声波衰减粘弹性及缺陷检测[J]东北工学院学报, 1993, 14(3):221~225.
[58]李造鼎.岩石中孔隙流体含量对超声波衰减影响的实验研究[J],应用声学,1987, 6(4): 35~38.
[59]李造鼎.双轴压缩下干燥与饱水岩石中超声波衰减的实验研究[J]应用声学,1988 7(2):10~15.
[60] Auberger M, Rinehart J S. Attenusation ofLongitudinal Waves in rocks[J]. J. G.R,1960,86(1):191~199.
[61]蔡忠理.超声波谱法在岩石破裂特性研究中的应用[J].岩土工程学报,1989, 11(3): 60~69.
[62]孙永联.声波波谱技术在采矿工程中的应用研究[J].岩石力学与工程学报,1993, 12(2): 115~125.
[63]周楚良.声波技术的进展及其在矿山压力测试中的应用[J].中国矿业大学学报,1991,20(3):12~21,
[64]蔡忠理.用声宵方法研究中间主应力对岩石破裂特性的影响[J]岩土工程学报,1992,13(2):116~121
[65]罗津辉.用声波参数确定岩石加载破坏过程的不同阶段[J].岩土力学,1992,13(1):51~56.