Seismic wave attenuation and dispersion resulting from wave-induced flow in porous rocks—A review
One major cause of elastic wave attenuation in heterogeneous porous media is wave-
induced flow of the pore fluid between heterogeneities of various scales. It is believed that …
induced flow of the pore fluid between heterogeneities of various scales. It is believed that …
A review of wave motion in anisotropic and cracked elastic-media
S Crampin - Wave motion, 1981 - Elsevier
Recent developments in the theory and calculation of wave propagation in anisotropic
media have been published in the geophysical literature and refer specifically to …
media have been published in the geophysical literature and refer specifically to …
[BOOK][B] Physical properties of rocks: fundamentals and principles of petrophysics
JH Schön - 2015 - books.google.com
The interpretation of geophysical data in exploration geophysics, well logging, engineering,
mining and environmental geophysics requires knowledge of the physical properties of …
mining and environmental geophysics requires knowledge of the physical properties of …
[BOOK][B] Practical handbook of physical properties of rocks and minerals (1988)
RS Carmichael - 2017 - books.google.com
CRC Practical Handbooks are a series of single-volume bench manuals that feature a
synthesis of the most frequently used, basic reference information. These highly abridged …
synthesis of the most frequently used, basic reference information. These highly abridged …
[BOOK][B] Seismic wave propagation and scattering in the heterogeneous earth
The structure of the earth has been extensively studied using seismic waves generated by
natural earthquakes and man-made sources. In classical seismology, the earth is …
natural earthquakes and man-made sources. In classical seismology, the earth is …
Constant Q‐wave propagation and attenuation
E Kjartansson - Journal of Geophysical Research: Solid Earth, 1979 - Wiley Online Library
A linear model for attenuation of waves is presented, with Q, or the portion of energy lost
during each cycle or wavelength, exactly independent of frequency. The wave propagation …
during each cycle or wavelength, exactly independent of frequency. The wave propagation …
Empirical relations between rock strength and physical properties in sedimentary rocks
In this study, 31 empirical equations are summarized that relate unconfined compressive
strength and internal friction angle of sedimentary rocks (sandstone, shale, and limestone …
strength and internal friction angle of sedimentary rocks (sandstone, shale, and limestone …
Seismic attenuation due to wave‐induced flow
Three P wave attenuation models for sedimentary rocks are given a unified theoretical
treatment. Two of the models concern wave‐induced flow due to heterogeneity in the elastic …
treatment. Two of the models concern wave‐induced flow due to heterogeneity in the elastic …
Transmission of seismic waves across single natural fractures
LJ Pyrak‐Nolte, LR Myer… - Journal of Geophysical …, 1990 - Wiley Online Library
Fractures and other nonwelded contacts are important mechanical and hydrological features
of rock masses. Their effects on seismic wave propagation can be modeled as a boundary …
of rock masses. Their effects on seismic wave propagation can be modeled as a boundary …
Attenuation of shear-waves in the lithosphere for frequencies from 0.05 to 25 Hz
K Aki - Physics of the Earth and Planetary Interiors, 1980 - Elsevier
Q for shear-waves in the crust and upper mantle was determined as a function of frequency
in the range 1–25 Hz, using band-pass filtered records of about 900 earthquakes occurring …
in the range 1–25 Hz, using band-pass filtered records of about 900 earthquakes occurring …