
The closed-form analytical expressions for the displacements and strains due to Tensile Dislocation (TD) located in a homogeneous, isotropic poroelastic half-space are obtained. The variation of radial displacement and strains with epicentral distance for the various materials Ruhr Sandstone, Tennessee Marble, Charcoal Granite, Berea Sandstone and Westerly Granite are discussed.
Poroelastic half-space, displacement, epicentral distance, Tensile Dislocation
Poroelastic half-space, displacement, epicentral distance, Tensile Dislocation
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