Implications on 1 + 1 D Tsunami Runup Modeling due to Time Features of the Earthquake Source

2018 ◽  
Vol 175 (4) ◽  
pp. 1393-1404 ◽  
Author(s):  
M. Fuentes ◽  
S. Riquelme ◽  
J. Ruiz ◽  
J. Campos
Keyword(s):  
Earthquake Source ◽  
Tsunami Runup

EARTHQUAKE SOURCE PARAMETER AND FOCAL MECHANISM ESTIMATES FOR THE WESTERN QUEBEC SEISMIC ZONE IN EASTERN CANADA

2017 ◽  
Author(s):  
Alba M. Rodriguez Padilla ◽  
◽  
John Onwuemeka ◽  
John Onwuemeka ◽  
Yajing Liu ◽  
...  
Keyword(s):  
Focal Mechanism ◽  
Earthquake Source ◽  
Source Parameter ◽  
Seismic Zone ◽  
Eastern Canada

scholarly journals A rapid estimation of near‐field tsunami runup

2015 ◽  
Vol 120 (9) ◽  
pp. 6487-6500 ◽  
Author(s):  
Sebastián Riquelme ◽  
Mauricio Fuentes ◽  
Gavin P. Hayes ◽  
Jaime Campos
Keyword(s):  
Near Field ◽  
Rapid Estimation ◽  
Tsunami Runup

The solution of the dynamic field of the Haskell fault model reconsidered

1982 ◽  
Vol 72 (4) ◽  
pp. 1069-1083
Author(s):  
R. D. List
Keyword(s):  
Half Space ◽  
Displacement Field ◽  
Body Force ◽  
Fault Model ◽  
Earthquake Source ◽  
Infinite Space ◽  
Force Method ◽  
Body Force Method ◽  
Rupture Speed ◽  
Seismic Dislocations

abstract A method of obtaining the displacement field of the Haskell model of an earthquake source, based on the well-known equivalence of seismic dislocations and body force, is described. It is shown that the solution of Madariaga (1978) can be generalized and that the two methods are equivalent for the problem of a rectangular dislocation expanding on a plane in an infinite space with a variable rupture speed and variable slip in the direction of rupture. One of the advantages of the equivalent body force method is that it can be used to readily obtain the transformed solution to the Haskell model in a half-space for a rectangular dislocation, expanding with variable rupture speed and variable slip.

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