Transmission of seismic waves across single natural fractures
Abstract
Fractures and other nonwelded contacts are important mechanical and hydrological features of rock masses. Their effects on seismic wave propagation can be modeled as a boundary condition in the seismic wave equation. Seismic stress is continuous across such a boundary, but seismic particle displacement and seismic particle velocity are not. The complete solutions for seismic wave reflection, conversion, and transmission across a displacement and...
Paper Details
Title
Transmission of seismic waves across single natural fractures
Published Date
Jun 10, 1990
Volume
95
Pages
8617 - 8638
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