Ground deformation due to interaction between infinite and finite dip-slip fault in a viscoelastic half-space of standard linear solid (SLS)
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences,General Environmental Science
Link
https://link.springer.com/content/pdf/10.1007/s12517-022-10311-2.pdf
Reference27 articles.
1. Baziar MH, Nabizadeh A, Jabbary M (2014) Numerical modeling of interaction between dip-slip fault and shallow foundation, Bull Earthquake Eng. 10.1007/s10518-014-9690-1
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3. Caporali A, Floris M, Chen X, Nurce B, Bertocco M, Zurutuza J (2020) The November 2019 seismic sequence in Albania: Geodetic constraints and fault interaction. Remote Sens 12. https://doi.org/10.3390/rs12050846
4. Cohen SC (1992) Postseismic deformation and stress diffusion due to visco-elasticity and comments on the modified Elsasser model. J Geophys Res 97:15395–15403
5. Crider JG, Pollard DD (1998) Fault linkage: Three-dimensional mechanical interaction between echelon normal faults. J Geophys Res 103(B10):24373–24391
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1. Determination of effect of the movement of an infinite fault in viscoelastic half space of standard linear solid using fractional calculus;Physica Scripta;2022-11-21
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