Abstract
A new computational model is proposed for propagation of low-amplitude seismic waves through a pre-stressed anisotropic medium. The model provides clues to kinematics and dynamics of these waves forming under the effect of initial stress. The governing differential equations are formulated in terms of velocity, stress tensor and small rotation of an element of the medium. The equations are solved numerically by means of the rotated staggered-grid method, and the approach is tested in numerical examples.
Sign-in/Register to access full text options 
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 callDisclaimer: 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.
