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The method makes it possible to predictLATat the receiver, located beyond the shadow zone that is caused by upward refraction.
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Beyond this depth and around the shadow zone, low-velocity incursions were observed.
Consequently, these reflection distortions observed beyond 3 s, especially within the shadow zone, are attributed to multiple reflected seismic events.
Despite the shadow zone of overlap, the distinction is there.
Critical value for the shadow zone.
Therefore, the shadow zone is created also by this target.
And hence, T-B creathe the shadow zone, too.
If a person creating the shadow zone is moving, then the shadow zone is space and time variables.
However, reflection events within the shadow zone appear enhanced than the initial PSDM, but the shadow effect is still evident.
Migrating with the primary velocities accounted for the primary reflections away from the shadow zone.
According to the motion states of the tracked persons, the shadow zone can take two forms.
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