Elastic Dispersion and Attenuation in Fully Saturated Sandstones: Role of Mineral Content, Porosity, and Pressures-Reference-Cited by-同舟云学术

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Elastic Dispersion and Attenuation in Fully Saturated Sandstones: Role of Mineral Content, Porosity, and Pressures

Published:2017-12 Issue:12 Volume:122 Page:9950-9965
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Pimienta Lucas¹²^ORCID,Borgomano Jan V. M.¹^ORCID,Fortin Jérôme¹,Guéguen Yves¹

Affiliation:

1. Laboratoire de Géologie de l'ENS - PSL Research University - UMR8538 du CNRS; Paris France

2. Laboratory of Experimental Rock Mechanics; Ecole Polytechnique Fédérale de Lausanne; Lausanne Switzerland

Funder

Total

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2017JB014645/fullpdf

Reference56 articles.

1. Dispersion of elastic moduli in a porous-cracked 431 rock: Theoretical predictions for squirt-flow;Adelinet;Tectonophysics,2011

2. Frequency and fluid effects on elastic properties of basalt: Experimental investigations;Adelinet;Geophysical Research Letters,2010

3. Modelling ultrasonic laboratory measurements of the saturation dependence of elastic modulus: New insights and implications for wave propagation mechanisms;Amalokwu;International Journal of Greenhouse Gas Control,2017

4. Fluids and frequency dependent seismic velocity of rocks;Batzle;The Leading Edge,2001

5. Fluid mobility and frequency-dependent seismic velocity-direct measurements;Batzle;Geophysics,2006

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