Attenuation and velocities of P-and S-waves in dry and saturated crystalline and sedimentary rocks at ultrasonic frequencies

Physics and Chemistry of the Earth

Volumn 22, Issue 1-2 SPEC. ISS., 1997, Pages 75-79

  Liu, B ^a,b   Kern, H ^a   Popp, T ^a  

^a UNIVERSITY OF KIEL   (Germany)

^b UNIVERSITY OF SCIENCE AND TECHNOLOGY OF CHINA   (China)

Author keywords

[No Author keywords available]

Indexed keywords

ATTENUATION; SEISMIC VELOCITY; SILICATE ROCK;

EID: 0031419940     PISSN: 00791946     EISSN: None     Source Type: Journal    
DOI: 10.1016/s0079-1946(97)00081-5     Document Type: Article

References (5)

1. Johnston, D.H., and Toksöz, M.N., Ultrasonic P and S wave attenuation in dry and saturated rocks under pressure, Journal of Geophys. Res., 85 (32), 925-936, 1980.
2. Kern, H., P-and S-wave velocities in crustal and mantle rocks under the simultaneous action of high confining pressure and high temperature and the effect of the rock micro-structure, In: W. Schreyer, High Pressure Researches in Geoscience, Stuttgart: Schweizerbart'sche. 15-45, 1982.
3. Kern, H. , Liu, B. and Popp, T., Relationship between anisotropy of P-and S-wave velocities and anisotropy of attenuation in serpentinite and amphibolite (submitted to JGR).
4. Meissner, R., The continental crust - a geophysical approach, Intern. Geophys. Ser., Academic Press, 426, 1986.
5. Winkler, K.W. and Nur, A., Seismic attenuation: effects of pore fluids and frictional sliding, Geophysics, 47, 1-15, 1982.