FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2148548049> ?p ?o ?g. }

• W2148548049 endingPage "582" @default.
• W2148548049 startingPage "568" @default.
• W2148548049 abstract "We present an analytic solution in the Fourier domain for an elastic deformation in a semi-infinite solid due to an arbitrary surface traction. We generalize the so-called Boussinesq's and Cerruti's problems to include a restoring buoyancy boundary condition at the surface. Buoyancy due to a large density contrast at the Earth's surface is an approximation to the full effect of gravity that neglects the perturbation of the gravitational potential and the change in density in the interior. Using the perturbation method, and assuming that the effect of gravity is small compared to the elastic deformation, we derive an approximation in the space domain to the Boussinesq's problem that accounts for a buoyancy boundary condition at the surface. The Fourier- and space-domain solutions are shown to be in good agreement. Numerous problems of elastostatic or quasi-static time-dependent deformation relevant to faulting in the Earth's interior (including inelastic deformation) can be modelled using equivalent body forces and surface tractions. Solving the governing equations with the elastic Green's function in the space domain can be impractical as the body force can be distributed over a large volume. We present a computationally efficient method to evaluate the elastic deformation in a 3-D half space due to the presence of an arbitrary distribution of internal forces and tractions at the surface of the half space. We first evaluate the elastic deformation in a periodic Cartesian volume in the Fourier domain, then use the analytic solutions to the generalized Boussinesq's and Cerruti's problems to satisfy the prescribed mixed boundary condition at the surface. We show some applications for magmatic intrusions and faulting. This approach can be used to solve elastostatic problems involving spatially heterogeneous elastic properties (by employing a homogenization method) and time-dependent problems such as non-linear viscoelastic relaxation, poroelastic rebound and non-steady fault creep under the assumption of spatially homogeneous elastic properties." @default.
• W2148548049 created "2016-06-24" @default.
• W2148548049 creator A5007517656 @default.
• W2148548049 creator A5032374728 @default.
• W2148548049 date "2010-06-23" @default.
• W2148548049 modified "2023-10-04" @default.
• W2148548049 title "Fourier-domain Green's function for an elastic semi-infinite solid under gravity, with applications to earthquake and volcano deformation" @default.
• W2148548049 cites W1987651695 @default.
• W2148548049 cites W1992320266 @default.
• W2148548049 cites W1994576411 @default.
• W2148548049 cites W1999885395 @default.
• W2148548049 cites W2000058411 @default.
• W2148548049 cites W2014217151 @default.
• W2148548049 cites W2026482913 @default.
• W2148548049 cites W2028084852 @default.
• W2148548049 cites W2031967575 @default.
• W2148548049 cites W2038413783 @default.
• W2148548049 cites W2046171065 @default.
• W2148548049 cites W2065958855 @default.
• W2148548049 cites W2070272760 @default.
• W2148548049 cites W2078798630 @default.
• W2148548049 cites W2083208183 @default.
• W2148548049 cites W2089384524 @default.
• W2148548049 cites W2091000291 @default.
• W2148548049 cites W2108593305 @default.
• W2148548049 cites W2112109708 @default.
• W2148548049 cites W2118408741 @default.
• W2148548049 cites W2122267972 @default.
• W2148548049 cites W2125035548 @default.
• W2148548049 cites W2130014760 @default.
• W2148548049 cites W2131772989 @default.
• W2148548049 cites W2137433526 @default.
• W2148548049 cites W2141341915 @default.
• W2148548049 cites W2146564568 @default.
• W2148548049 cites W2152927701 @default.
• W2148548049 cites W2157396881 @default.
• W2148548049 cites W2163324778 @default.
• W2148548049 cites W2168762126 @default.
• W2148548049 cites W2170931233 @default.
• W2148548049 cites W2171701436 @default.
• W2148548049 cites W2395841650 @default.
• W2148548049 cites W3016180305 @default.
• W2148548049 cites W3112597099 @default.
• W2148548049 cites W4211220323 @default.
• W2148548049 cites W4249050009 @default.
• W2148548049 doi "https://doi.org/10.1111/j.1365-246x.2010.04655.x" @default.
• W2148548049 hasPublicationYear "2010" @default.
• W2148548049 type Work @default.
• W2148548049 sameAs 2148548049 @default.
• W2148548049 citedByCount "65" @default.
• W2148548049 countsByYear W21485480492012 @default.
• W2148548049 countsByYear W21485480492013 @default.
• W2148548049 countsByYear W21485480492014 @default.
• W2148548049 countsByYear W21485480492015 @default.
• W2148548049 countsByYear W21485480492016 @default.
• W2148548049 countsByYear W21485480492017 @default.
• W2148548049 countsByYear W21485480492018 @default.
• W2148548049 countsByYear W21485480492019 @default.
• W2148548049 countsByYear W21485480492020 @default.
• W2148548049 countsByYear W21485480492021 @default.
• W2148548049 countsByYear W21485480492022 @default.
• W2148548049 countsByYear W21485480492023 @default.
• W2148548049 crossrefType "journal-article" @default.
• W2148548049 hasAuthorship W2148548049A5007517656 @default.
• W2148548049 hasAuthorship W2148548049A5032374728 @default.
• W2148548049 hasBestOaLocation W21485480491 @default.
• W2148548049 hasConcept C102519508 @default.
• W2148548049 hasConcept C114793014 @default.
• W2148548049 hasConcept C121332964 @default.
• W2148548049 hasConcept C127313418 @default.
• W2148548049 hasConcept C134306372 @default.
• W2148548049 hasConcept C153294291 @default.
• W2148548049 hasConcept C204366326 @default.
• W2148548049 hasConcept C207864730 @default.
• W2148548049 hasConcept C2524010 @default.
• W2148548049 hasConcept C33923547 @default.
• W2148548049 hasConcept C38834483 @default.
• W2148548049 hasConcept C538625479 @default.
• W2148548049 hasConcept C57879066 @default.
• W2148548049 hasConcept C74650414 @default.
• W2148548049 hasConcept C91588493 @default.
• W2148548049 hasConcept C9358284 @default.
• W2148548049 hasConceptScore W2148548049C102519508 @default.
• W2148548049 hasConceptScore W2148548049C114793014 @default.
• W2148548049 hasConceptScore W2148548049C121332964 @default.
• W2148548049 hasConceptScore W2148548049C127313418 @default.
• W2148548049 hasConceptScore W2148548049C134306372 @default.
• W2148548049 hasConceptScore W2148548049C153294291 @default.
• W2148548049 hasConceptScore W2148548049C204366326 @default.
• W2148548049 hasConceptScore W2148548049C207864730 @default.
• W2148548049 hasConceptScore W2148548049C2524010 @default.
• W2148548049 hasConceptScore W2148548049C33923547 @default.
• W2148548049 hasConceptScore W2148548049C38834483 @default.
• W2148548049 hasConceptScore W2148548049C538625479 @default.
• W2148548049 hasConceptScore W2148548049C57879066 @default.
• W2148548049 hasConceptScore W2148548049C74650414 @default.
• W2148548049 hasConceptScore W2148548049C91588493 @default.
• W2148548049 hasConceptScore W2148548049C9358284 @default.

• next