Analytical seismic wave attenuation and velocity dispersion in layered double-porosity media

[摘要] Due to differences of rock properties such as porosity, permeability and compressibility between different regions in the porous media, pressure gradients are induced between those different regions and lead to local fluid flow. When seismic wave propagat

[学科分类] 地球化学与岩石

[关键词] local fluid flow