True
False
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VSP survey takes into account of upgoing energy whereas checkshot survey takes into account of the downgoing energy.
Only checkshot survey calibrates with the sonic log in order to correct for any erroneous velocity.
A check shot velocity survey measures a much larger cylindrical volume of rock compared to VSP survey.
Only the first directly arriving signals sensed by the downhole geophone in a checkshot survey whereas VSP takes account of both reflected and direct arrival signals.
True
False
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Constructive, positive, one-third
Constructive, positive, one-quarter
Constructive, destructive, one-third
Constructive, destructive, one-quarter
Changes in signal-to-noise ratio in the data
Changes in acoustic impedance, e.g. shale overlies on a gas sand
Changes in tuning effect
Changes in lithology
RMS velocity is that of a wave that travels through subsurface layers of similar interval velocity along a specific raypath whereas stacking velocity is velocity calculated from velocity analysis based on normal-moveout measurements.
RMS velocity is that of a wave that travels through subsurface layers of different interval velocity along a specific raypath whereas stacking velocity is velocity calculated from velocity analysis based on normal-moveout measurements.
RMS velocity is that of a wave that travels through subsurface layers of different interval velocity along a specific raypath whereas stacking velocity is velocity calculated from varying constant models based on normal-moveout measurements.
The stacking velocity and the root-mean-square velocity approach equality when the layers are horizontal and isotropic.
The stacking velocity and the root-mean-square velocity approach equality when source-receiver offset approaches zero and layers are horizontal and isotropic.
The stacking velocity and the root-mean-square velocity approach equality when the velocities in the subsurface layers are varying horizontally only (not vertically).
The stacking velocity and the root-mean-square velocity approach equality when the velocities in the subsurface layers are varying vertically only (not horizontally).
Humble Formula
Dix Formula
Zoeppritz Equation
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Well-to-seismic tie
Attribute extraction
Volume scanning
Gathers analysis
Invasion effects
Poor seismic data quality
Erroneous sonic logs
The acoustic impedances of sands and shales are quite similar
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