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The particle settling velocity model of Ganser (1993) was used to predict settling rates of particles.
The required radio-wave velocity model varies with depth using a depth density parameterization53 and a density velocity relation54.
The strongly simplified Settling Velocity Model (SVM) is also tested.
Modeling of ground motion from a 1994 Northridge aftershock using a tomographic velocity model of the Los Angeles basin, Bull.
In addition, direct stacking removes any wave type assumption or velocity model dependence, making it useful for detecting both local and distant events.
Eberhart-Phillips, D., Reyners, M., Bannister, S., Chadwick, M. & Ellis, S. Establishing a versatile 3-D seismic velocity model for New Zealand.
With proper time shifts predicted by an assumed location and 1D velocity model, stacking of local similarity is expected to be more constructive.
Issues related to the conditional velocity model are discussed.
Hence, it does not require a symmetric discrete velocity model.
The velocity model can be considered an "equivalent" velocity model.
1D velocity model interpolated from CRUST2.0.
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