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Chinese Journal of High Pressure Physics  > 2002  >  16(3): 176-182 .
YUE Lan-Xiu, XIE Hong-Sen, LIU Cong-Qiang, WU Feng-Chang. Compressional Velocity and Attenuation in Amphibolite at 2.0 GPa and up to 1 200 ℃[J]. Chinese Journal of High Pressure Physics, 2002, 16(3): 176-182 . doi: 10.11858/gywlxb.2002.03.003
Citation: YUE Lan-Xiu, XIE Hong-Sen, LIU Cong-Qiang, WU Feng-Chang. Compressional Velocity and Attenuation in Amphibolite at 2.0 GPa and up to 1 200 ℃[J]. Chinese Journal of High Pressure Physics, 2002, 16(3): 176-182 . doi: 10.11858/gywlxb.2002.03.003
shu

Compressional Velocity and Attenuation in Amphibolite at 2.0 GPa and up to 1 200 ℃

doi: 10.11858/gywlxb.2002.03.003
  • 1.

    Institute of Geochemistry, Chinese Academy of Science, Guiyang 550002, China;

  • 2.

    Graduate School of Chinese Academy of Sciences, Beijing 100039, China

More Information
  • Corresponding author: YUE Lan-Xiu
  • Received Date: 16 Jan 2002
  • Rev Recd Date: 30 Mar 2002
  • Publish Date: 05 Sep 2002
    Abstract
  • Compressional wave velocity and attenuation in amphibolite collected from Kudi, Xinjiang Province were measured at high pressure (2.0 GPa) and high temperature (up to 1 200 ℃). The experimental results show that vp and Q values decrease with the increase of temperature. At the beginning of increasing temperature, vp decreases slowly, and then decreases rapidly with the higher temperature. Because of amphiboliteps anisotropy, the temperature at which vp decreases quickly in different directions is different. The temperature is 812 ℃ in x and y and 673 ℃ in z. However, the temperature at which Q decreases quickly is about 812 ℃ at the three directions. It can be concluded from the experimental results of minerals that as the temperature is higher than 647 ℃, the melt appears. The scope of vp decreasing with temperature in x and y directions is not various than before. It increases in z direction. However, the melt does not affect Q values. As the temperature is higher than 812 ℃, the melt is more than before, vp and Q values decrease more quickly. Therefore, partial melting is the main reason for elastic wave velocity decreasing and attenuation increasing.

     

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    • References(39)
  • Birch F. The Velocity of Compressional Waves in Rocks to 10 Kilobars [J]. J Geophys Res, 1960, 65: 1083-1102.
    Gordon R B, Davis L A . Velocity and Attenuation of Seismic Waves in Imperfectly Elastic Rock [J]. J Geophys Res, 1968, 73: 3917-3935.
    Jackson D D, Anderson D L. Physical Mechanisms of Seismic Wave Attenuation [J]. Rev Geophys Space Phys, 1970, 8: 1-63.
    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.
    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.
    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.
    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.
    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)
    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.
    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)
    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.
    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)
    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.
    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)
    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.
    Murase T, Kushiro I. Compressional Wave Velocity in Partially Molten Peridotite at High Pressure [J]. Carnegie Inst Wash YB, 1979, 78: 559-562.
    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)
    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.
    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)
    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.
    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)
    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.
    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.
    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)
    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.
    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)
    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.
    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)
    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.
    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)
    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.
    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.
    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)
    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.
    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.
    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.
    Biot M A. Mechanics of Deformation and Acoustic Propagation in Porous Media [J]. J Appl Phys, 1962, 33(4): 1482-1498.
    Mavko G M, Nur A. Wave Attenuationin Partially Saturated Rocks [J]. Geophysics, 1979, 44 (1): 161-178.
    Yamakawa N. Scattering and Attenuation of Elastic Waves [J]. Geophys Mag, 1962, 31(1): 61-103.
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