Water bottom multiple
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Three successive rebounds within the water layer, if not more, are visible and can be readily accounted for. The two interfaces, at either side of the water level, are excellent reflector.. In some areas, there occur anomalous up-hole times which are difficult to explain http. The marine section illustrated on Plate 56, from offshore Labrador, shows this kind of multiple.
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Seismic Methods And Applications
Plate The reverberation in water illustrated on this sketch corresponds to persistence of a wave sound after its source has stopped, caused by multiple reflection of the wave within a closed space in this case the water layer. Reflected refractions contain information only about the refractor. The two interfaces, at either side of the water level, are excellent reflector.. This is particularly true, on hard water-bottom areas where sediments are compacted and well consolidated. A reflection event arriving a short time after the primary from the surface or the base of weathered layer buried explosion on land. A strong reflection, culminating at approximately 2 seconds, is visible in the middle of the section. Admittedly, this line is affected by numerous multiples.
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Assuming a constant avo water
However, this is not always the case. Plate Multiply reflected seismic energy or any event in seismic data that has incurred more than one reflection in its travel path is considered a multiple. In addition to rays that return to the surface after reflection at single interface, known as primary reflection , there are many paths in a layered subsurface by which rays may return to the surface after reflection at more than one interface Plate As illustrated a peg leg multiple is a type of short-path multiple, or multiply-reflected seismic energy, which has an asymmetric path. Reflected refractions contain information only about the refractor. Diffraction refers to various phenomena which occur when a wave encounters an obstacle. Plate The reverberation in water illustrated on this sketch corresponds to persistence of a wave sound after its source has stopped, caused by multiple reflection of the wave within a closed space in this case the water layer.
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