Ultrasonic compressional and shear velocities in dry clastic rocks as a function of porosity, clay content, and confining pressure

Details Ultrasonic compressional and shear velocities in dry clastic rocks as a function of porosity, clay content, and confining pressure Ultrasonic compressional and shear velocities in dry clastic rocks as a function of porosity, clay content, and confining pressure

Jan 1992

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992geoji.108..125f&link_type=ejournal

Geophysical Journal International, vol. 108, issue 1, pp. 125-135

Physics

20

Scientific paper

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