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Azimuth is the bearing from the source to the receiver
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Azimuth is the bearing from the source to the receiver.
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85081453485
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A bin is the area on the target surface, typically 25 m by 25 m [82 ft by 82 ft], to which seismic traces are assigned according to their common midpoint (CMP).
-
A bin is the area on the target surface, typically 25 m by 25 m [82 ft by 82 ft], to which seismic traces are assigned according to their common midpoint (CMP).
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Stacking is the summation of signals, and is performed to enhance signal-to-noise ratio
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Stacking is the summation of signals, and is performed to enhance signal-to-noise ratio.
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Michell, S.1
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Wave-equation migration uses a velocity model and various solutions to the wave equation that describe propagation of waves through rock. The objective is to redistribute reflected seismic energy from its assumed position at the source-receiver midpoint to its true position
-
Wave-equation migration uses a velocity model and various solutions to the wave equation that describe propagation of waves through rock. The objective is to redistribute reflected seismic energy from its assumed position at the source-receiver midpoint to its true position.
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24
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85081446715
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Multiclient surveys are surveys acquired by seismic contractors over unlicensed areas, then made available to multiple clients. Partial funding for multiclient surveys may be provided by one or more E&P companies
-
Multiclient surveys are surveys acquired by seismic contractors over unlicensed areas, then made available to multiple clients. Partial funding for multiclient surveys may be provided by one or more E&P companies.
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25
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85081452129
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A salt keel is what remains of the root of an intruding salt body after the root has detached itself from the parent salt layer
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A salt keel is what remains of the root of an intruding salt body after the root has detached itself from the parent salt layer.
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Polarity of a seismic signal refers to the direction of its amplitude in a recorded seismic trace. Negative and positive amplitudes have opposite polarity
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Polarity of a seismic signal refers to the direction of its amplitude in a recorded seismic trace. Negative and positive amplitudes have opposite polarity.
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Low-frequency information is needed for inversion of seismic data because typically, the seismic data themselves provide only high-frequency information, such as relative changes in reflectivity or acoustic impedance at each layer boundary. Low-frequency information, typically derived from checkshots or integrated sonic logs, provides trie baseline from which the high-frequency data vary. By combining both low-and high-frequency information, absolute changes in rock properties may be calculated. Because seismic inversion requires a combination of seismic and well data, it usually cannot be performed reliably in the absence of wells. However, if seismic data could be acquired with low-frequency content intact, inversion could be carried out in more areas
-
Low-frequency information is needed for inversion of seismic data because typically, the seismic data themselves provide only high-frequency information, such as relative changes in reflectivity or acoustic impedance at each layer boundary. Low-frequency information, typically derived from checkshots or integrated sonic logs, provides trie baseline from which the high-frequency data vary. By combining both low-and high-frequency information, absolute changes in rock properties may be calculated. Because seismic inversion requires a combination of seismic and well data, it usually cannot be performed reliably in the absence of wells. However, if seismic data could be acquired with low-frequency content intact, inversion could be carried out in more areas.
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