AGU Ref Shelf. Rock Physics and Phase Relations by T. Ahrens PDF

By T. Ahrens

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41]. Dotted lines are reference values for gas, oil, and water. Additional information can be found by correlating velocities with other rock properties, such as density derived from nuclear well logs. When velocities are measured as continuous functions of depth in wellbores, the data can be integrated to yield the total acoustic traveltime to any depth, thereby providing depth calibration for surface reflection seismograms. The VP/V, ratio is often 0 5 Angle 10 15 20 of Incidence 35 (degrees) Fig.

Geophys. , 32 9. IO. Il. 12. 13. 14. 15. 16. 17. 18. 19. ACOUSTIC VELOCITY AND ATI’ENUATION 65, 1083,196O. , The velocity of compressional waves in rocks to IO kilobars, Part 2, J. Geophys. Res.. , Shear wave birefringence in dilating granite, Geophys. Res. , I, 217, 1974. W. Paulding, and C. Scholz, Dilatancy in the fracture of crystalline rocks, J. Geophys. , 71, 3939,1966. , 0. Coussy, and B. , 1987. , Predicting relative and absolute variations of in-situ permeability from full-waveform acoustic logs, The Log Analyst, 32, 246,199l.

Additional examplesof construction of a theoretical Hugoniot from constituentmineralsare given in [6] and [4]. T. J. Ahrens and M. L. Johnson, Seismological Laboratory, 252-21, California Instihrte of Technology, Pasadena, CA 91125 1995 by the American (lb) where p. This approachworks well in the high pressureregime (4, of Fig. 2). More successfulover the pressure range of the entire Hugoniot is the mineral mixture model [S]. OF STATE Rocks are, by definition, composed of one or more minerals, and hence largely their equation of state behavior (Table 1) reflects the behavior of their constitutive minerals.

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AGU Ref Shelf. Rock Physics and Phase Relations by T. Ahrens

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