Deformation of an Elastic-Layer Overlying an Elastic Half-Space Caused by a Finite, Buried, Inclined, Locked Strike-Slip Fault

2021 ◽  
pp. 283-306
Author(s):  
Piu Kundu ◽  
Seema Sarkar (Mondal)
Keyword(s):  
Half Space ◽  
Elastic Layer ◽  
Elastic Half Space ◽  
Strike Slip ◽  
Strike Slip Fault

On strike-slip Somigliana dislocations in a layered elastic half-space

1983 ◽  
Vol 6 (3) ◽  
pp. 261-270 ◽  
Author(s):  
M. Dragoni ◽  
D. Golinelli
Keyword(s):  
Half Space ◽  
Elastic Half Space ◽  
Strike Slip

Stress relaxation in a semi-infinite viscoelastic earth model

1973 ◽  
Vol 63 (6-1) ◽  
pp. 2145-2154
Author(s):  
Martin Rosenman ◽  
Sarva Jit Singh
Keyword(s):  
Free Surface ◽  
Stress Relaxation ◽  
Half Space ◽  
Epicentral Distance ◽  
Strike Slip ◽  
Strike Slip Fault ◽  
Earth Model ◽  
Contour Maps ◽  
Surface Stresses ◽  
Stress Components

Abstract Expressions for quasi-static surface stresses resulting from a finite, rectangular, vertical, strike-slip fault in a Maxwellian viscoelastic half-space are derived. Variation of the stresses with time and epicentral distance is studied. Contour maps are obtained in some representative cases. It is found that all nonvanishing stress components at the free surface die exponentially with time. This is in contrast to the behavior of the displacements and strains which, in general, do not vanish for large times.

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