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Języki publikacji
Abstrakty
The relaxed rigidity method is used for calculating the postseismic deformation of an elastic layer (lithosphere) overlying a yiscoelastic half-space (asthenosphere) caused by a very long dip-slip fault in the layer. The integrals involved are evaluated approximately by replacing the integrand by a finite sum of exponential terms. Detailed numerical results showing the variation of the surface displacements with the epicentral distance for various source depths and for various values of the relaxed rigidity of the half-space are presented graphically.
Słowa kluczowe
Wydawca
Czasopismo
Rocznik
Tom
Strony
69--77
Opis fizyczny
Bibliogr. 8 poz.
Twórcy
autor
autor
autor
- Department of Mathematics, Maharshi Dayanand University, Rohtak India, sjsingh@mdul.ernet.in
Bibliografia
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BSL8-0002-0011