Dispersion in oceanic crust during earthquake preparation

DOI10.1016/S0020-7683(98)00160-7zbMath0954.74037OpenAlexW2078881272WikidataQ126351216 ScholiaQ126351216MaRDI QIDQ1302824

M. D. Sharma

Publication date: 8 February 2001

Published in: International Journal of Solids and Structures (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1016/s0020-7683(98)00160-7

zbMATH Keywords

Rayleigh wavesfrequency equationfluid layersurface wavesseismologyearthquakethree-layer systemStonely wavesdispersive effectaccumulation of stresseschanges in dispersion curvescracked elastic solidoceanic crusttransversely isotropic poroelastic layer

Mathematics Subject Classification ID

Related Items (2)

Dynamic Green's functions for a liquid layer overlying a transversely isotropic solid half-space due to an arbitrary source excitation within the liquid ⋮ Rigid disc vibration in a multi-layered transversely isotropic poroelastic half-space underlying a liquid layer

This page was built for publication: Dispersion in oceanic crust during earthquake preparation