Kern H, Liu B, Popp T. Relationship between Anisotropy of P and S Wave Velocities And Anisotropy of Attenuation in Serpentinite and Amphibolite [J]. J Geophys Res, 1997, 102(B2): 3051-3065.
[2]
Lebedev E B, Kern H. The Effect of Hydration and Dehydration Reactions on Wave Velocities in Basalts [J]. Tectonophysics, 1999, 308: 331-340.
[3]
Matsushima S. Partial Melting of Rocks Observed by the Sound Velocity Method and the Possibility of a Quasi -Dry Low Velocity Zone in the Upper Mantle [J]. Phys Earth Planet Inter, 1989, 55: 306-312.
[4]
Ito K. Effects of H2O on Elastic Wave Velocities in Ultrabasic Rocks at 900 ℃ under 1 GPa [J]. Phys Earth Planet Inter, 1990, 61: 260-268.
[5]
Kern H. Elastic-Wave Velocity in Crustal and Mantle Rocks at High Pressure and Temperature: The Role of the High-Low Quartz Transition and of Dehydration Reactions [J]. Phys Earth Planet Inter, 1982, 29: 12-23.
[6]
Popp T, Kern H. Thermal Dehydration Reactions Characterised by Combined Measurements of Electrical Conductivity and Elastic Wave Velocities [J]. Earth Planet Sci Lett, 1993, 120: 43-57.
[7]
Zhao Z D, Gao S, Luo T C, et al. Origin of the Crustal Low Velocity Layer of Qinling and North China: Evidence from Laboratory Measurement of P-Wave Velocity in Rocks at High p-T Conditions [J]. Acta Geophysica Sinica, 1996, 39(5): 637-652. (in Chinese)
Zhou W G, Xie H S, Zhao Z D, et al. Effect of the Phase Transition on the Compressional Wave Velocity for a Trachybasalt at High Temperature and High Pressure [J]. Chin Sci Bull, 1999, 44(15): 1415-1418.
[10]
Yue L X, Xie H S, Liu C Q, et al. Compressional Velocity and Attenuation in Amphibolite at 2. 0 GPa and up to 1200 ℃ [J]. Chinese Journal of High Pressure Physics, 2002, 16(3): 176-182. (in Chinese)
Liu W, Du J G, Bai L P, et al. Compressional Elastic Wave Velocities of Serpentinized Olivine-Bearing Pyroxenite up to 960 ℃ at 1. 0 GPa [J]. J Phys(Condensed Matter), 2002, 14: 11355-11358.
[13]
Liu W, Du J G, Bai L P, et al. Compressional Elastic Wave Velocities of Serpentinized Pyroxenite at High Pressures and High Temperatures and Its Geological Significance [J]. Acta Seismologica Sinica, 2002, 15(4): 456-461.
[14]
Tatsumi Y, Ito K, Goto A. Elastic Wave Velocites in Isochemical Granulite and Amphibolite: Origin of a Low-Velocity Layer at the Slab/Mantle Wedge Interface [J]. Geophys Res Lett, 1994, 21(1): 17-20.
[15]
Yue L X. The Study of Seismic Velocity and Attenuation of Eclogite and Amphibolite at High Temperature and High Pressure [D]. Guiyang: Master Thesis of Institute of Geochemistry, Chinese Academy of Science, 2001: 18. (in Chinese)
Xie H S, Zhang Y M, Xu H G, et al. A New Method of Measuring the Elastic Wave Velocity of Rocks and Minerals at High Pressures and High Temperatures and Its Significance [J]. Science in China, 1993, 36B(10): 1276-1280.
[18]
Xie H S. Introduction to Material Science of the Earth Interior [M]. Beijing: Science Press, 1997: 50. (in Chinese)
[19]
谢鸿森.地球物质科学导论 [M]. 北京: 科学出版社, 1997: 50.
[20]
Ito K, Tatsumi Y. Measurement of Elastic Wave Velocities in Granulite and Amphibolite Having Identical H2O-Free Bulk Compositions up to 850 ℃ at 1 GPa [J]. Earth Planet Sci Lett, 1995, 133: 255-264.
[21]
Kern H, Schenk V. Elastic Wave Velocity in Rocks from a Lower Crustal Section in Northern Alabria(Italy) [J]. Phys Earth Planet Inter, 1985, 40: 147-160.
[22]
Kern H, Tubia J M. Pressure and Temperature Dependence of P-and S-Wave Velocities, Seismic Anisotropy And Density of Sheared Rocks from the Alpujata Massif(Ronda Peridotites, Southern Spain) [J]. Earth Planet Sci Lett, 1993, 119: 191-205.