Abstract

Pore space, pore fluid and the solid minerals control both the seismic behavior and permeability of a rock. Ignoring changes in the mineral matrix, the pore space is used to explain many issues associated with stress, pore pressure, permeability and saturation. The pore space is modeled using a generalization of ideas presented in the paper by Schoenberg and Sayers (1995) to describe the stress, pore pressure, permeability and saturation effects upon seismic.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.