[1] Birch F. The Velocity of Compressional Waves in Rocks to 10 Kilobars [J]. J Geophys Res, 1960, 65: 1083-1102.
[2] Gordon R B, Davis L A . Velocity and Attenuation of Seismic Waves in Imperfectly Elastic Rock [J]. J Geophys Res, 1968, 73: 3917-3935.
[3] Jackson D D, Anderson D L. Physical Mechanisms of Seismic Wave Attenuation [J]. Rev Geophys Space Phys, 1970, 8: 1-63.
[4] Christensen N I. Compressional Wave Velocities in Rocks at High Temperature and Pressure, Critical Thermal Gradients, and Curstal Low-Velocity Zones [J]. J Geophys Rrs, 1979, 64: 6849-6857.
[5] Johnston D H, Toksoz M N. Ultrasonic P and S Wave Attenuation in Dry and Saturated Rocks under Pressure [J]. J Geophys Res, 1980, 85: 925-936.
[6] Kern H, Richter A. Temperature Derivatives of Compressional and Shear Wave Velocities in Crustal and Mantle Rocks at 6 kbar Confining Pressure [J]. J Geophys, 1981, 49(1): 47-56.
[7] Xu J, Zhang Y, Hou W, et al. Measurements of Ultrasonic Wave Velocities at High Temperature and High Pressure for Window Glass, Pyrophyllite, and Kimberlite up to 1400 ℃ and 5. 5 GPa [J]. High Temperature-High Pressure, 1994, 26(4): 375-384.
[8] ZHOU Wen-ge, XIE Hong-sen, ZHAO Zhi-dan, et al. Phase Transition of Trachy-Basalt and Its Influence to Compressional Wave Velocities on High Temprature and High Pressure [J]. Chinese Science Bulletin, 1999, 44(4): 424-427. ( in Chinese)
[9] 周文戈, 谢鸿森, 赵志丹, 等. 高温、高压下粗面玄武岩相变对其纵波速度影响的研究 [J]. 科学通报, 1999, 44(4): 424-427.
[10] ZHANG You-nan, MA Jin. Investigation on Compressional Wave Velocities of Mafic Rocks in Deep Crust [J]. Chinese Journal of Geophysics, 1997, 40: 221-230. ( in Chinese)
[11] 张友南, 马谨. 深部地壳镁铁质岩石波速的研究 [J]. 地球物理学报, 1997, 40: 221-230.
[12] BAI Wu-ming, MA Mai-ning, LIU Jiang-lin. Testing Study on Elastic Wave Velocities and Electrical Conductivity of Crustal Rocks. Chinese Journal of Rock [J]. Mechanics and Engineering, 2000, 19(suppl): 899-904. ( in Chinese)
[13] 白武明, 马麦宁, 柳江琳. 地壳岩石波速和电导率实验研究 [J]. 岩石力学与工程学报, 2000, 19(增刊): 899-904.
[14] ZHAO Zhi-dan, GAO Shan, LUO Ting-chuan, et al. Origin of Crustal Low Velocity Later of Qinling and North China: Evidence Form Laboratory Measurement of P-Wave Velocity in Rocks at High P-T Conditions [J]. Chinese Journal of Geophysics, 1996, 39(5): 642-652. ( in Chinese)
[15] 赵志丹, 高山, 骆庭川等. 秦岭和华北地区地壳低速层的成因探讨--岩石高温高压波速实验证据 [J]. 地球物理学报, 1996, 39(5): 642-652.
[16] Murase T, Kushiro I. Compressional Wave Velocity in Partially Molten Peridotite at High Pressure [J]. Carnegie Inst Wash YB, 1979, 78: 559-562.
[17] XIE Hong-sen, ZHANG Yue-ming, XU Hui-gang, et al. The New Measurement of Elastic Wave in Rock and Mineral and Its Significance [J]. Science in China, 1993, 23(8): 861-864. ( in Chinese)
[18] 谢鸿森, 张月明, 徐惠刚, 等. 高温超高压下测量岩石矿物弹性波速的新方法及其地学意义 [J]. 中国科学(B辑), 1993, 23(8): 861-864.
[19] ZHOU Wen-ge, XIE Hong-sen, LIU Yong-gang, et al. Travel Time Measurement in Tungsten Carbide Anvil under High Pressure [J]. Chinese Journal of High Pressure Physics, 2000, 14(3): 171-175. ( in Chinese)
[20] 周文戈, 谢鸿森, 刘永刚, 等. 高压下碳化钨压砧走时的测量 [J]. 高压物理学报, 2000, 14(3): 171-175.
[21] LIU Bin, GE Ning-jie, Kern H, et al. Velocities and Attenuation of P-and S-waves and Their Anisotropies in Serpentinite and Amphibolite under Different p-T Conditions [J]. Chinese Journal of Geophysics, 1998, 41(3): 371-381. ( in Chinese)
[22] 刘斌, 葛宁洁, Kern H, 等. 不同温压条件下蛇纹岩和角闪岩中波速和衰减的各向异性 [J]. 地球物理学报, 1998, 41(3): 371-381.
[23] Johnston D H, Tokson M N, Timur A. Attentuation of Seismic Waves in Dry and Saturated Rocks: II Mechanisms [J]. Geophysics, 1979, 44(4): 691-711.
[24] GONG Zi-zheng, HUA Jing-song, JING Fu-qian, et al. A New Measurement of Temprature Coefficient in Elastic Wave Velocity at High Pressure [J]. Chinese Journal of High Pressure Physics, 2000, 14(4): 241-246. ( in Chinese)
[25] 龚自正, 华劲松, 经福谦, 等. 高压下声速温度系数的一种新算法 [J]. 高压物理学报, 2000, 14(4): 241-246.
[26] LIU Bin. Relations of Elastic Wave Velocity and Attenuation and Their Anisotropies to the Fabric of Rocks under Different p-T Conditions [J]. Earth Science Frontiers, 2000, 7(1): 247-257. ( in Chinese)
[27] 刘斌. 不同温压下岩石弹性波速度、衰减及各向异性与组构的关系 [J]. 地学前缘, 2000, 7(1): 247-257.
[28] ZHAO Zhi-dan. The Velocity of the Rocks from Dabieshan, Huabei and Qingzang Parriea in Chinese: Its Implications for Crust-Mantle Recycling [D]. Beijing: China University of Geosciences, 1998. ( in Chinese)
[29] 赵志丹. 中国大别山、华北和青藏高原岩石弹性波速: 对岩石圈组成和壳-幔循环的启示 [D]. 北京: 中国地质大学, 1998.
[30] ZHAO Zhi-dan, XIE Hong-sen, ZHOU Wen-ge, et al. Density and P-Wave Velocity of the Eclogite from Dabieshan and Its Implications for Crust-Mantle Recycling [J]. Bulletin of Mineralogy Petrology and Geochemistry, 2001, 20(1): 6-10. ( in Chinese)
[31] 赵志丹, 谢鸿森, 周文戈, 等. 大别山榴辉岩的密度和波速及其对壳-幔循环的启示 [J]. 矿物岩石地球化学通报, 2001, 20(1): 6-10.
[32] Sato H, Manghnani M H. Utrasonic Measurements of vp and Qp: Relaxation Spectrum of Complex Modulus on Basalt Melts [J]. Phys Earth Planet Inte. , 1985, 41: 18-33.
[33] XIE Hong-sen, ZHOU Wen-ge, LI Yu-wen, et al. The Elastic Characteristics of Serpentinits Dehydration at High Temperature-High Pressure and Its Significance [J]. Chinese Journal of Geophysics, 2000, 43(6): 806-811. ( in Chinese)
[34] 谢鸿森, 周文戈, 李玉文, 等. 高温高压下蛇纹岩脱水的弹性特征及其意义 [J]. 地球物理学报, 2000, 43(6): 806-811.
[35] Kern H, Liu B, Popp T. Relationship between Anisotropy of P and S Wave Velocities and Anisotropy of Attenuation in Serpentinite and Amphibolite [J]. Journal of Geophysical Research, 1997, 102(B2): 3051-3065.
[36] Prasad M, Manghnani M H, Siegesmund S. Compressional Wave Velocity and Quality Factor Characteristies of Seleted KTB Core Samples [J]. Sxientific Drilling, 1994, 4: 227-231.
[37] Biot M A. Mechanics of Deformation and Acoustic Propagation in Porous Media [J]. J Appl Phys, 1962, 33(4): 1482-1498.
[38] Mavko G M, Nur A. Wave Attenuationin Partially Saturated Rocks [J]. Geophysics, 1979, 44 (1): 161-178.
[39] Yamakawa N. Scattering and Attenuation of Elastic Waves [J]. Geophys Mag, 1962, 31(1): 61-103.