CPG Exploration Techniques & Seismic Interpretation 2 — Questions and Answers
Question 1: What does a flat spot on a seismic section typically indicate?
- A horizontal fluid contact such as a gas-water or oil-water interface (Correct answer)
- A uniform lithology with no impedance contrast
- The base of the salt body
- A processing artifact from stacking
Correct answer: A horizontal fluid contact such as a gas-water or oil-water interface
Flat spots are horizontal reflections that cross stratigraphic dip and represent fluid contacts where acoustic impedance changes at the phase boundary.
Question 2: In seismic stratigraphy, what is an 'onlap' configuration?
- Reflectors terminate against an underlying surface in an up-dip direction (Correct answer)
- Reflectors terminate against an overlying surface
- Reflectors converge and thin toward a structural high
- Reflectors are truncated by erosion at the top
Correct answer: Reflectors terminate against an underlying surface in an up-dip direction
Onlap occurs when initially horizontal or inclined strata terminate progressively against an inclined surface in an updip direction, indicating transgression or basin filling.
Question 3: Which seismic attribute is most directly related to pore fluid type?
- Poisson's ratio derived from Vp/Vs ratio (Correct answer)
- Acoustic impedance from P-wave velocity alone
- Dominant frequency of the wavelet
- NMO velocity from stacking
Correct answer: Poisson's ratio derived from Vp/Vs ratio
Poisson's ratio (derived from the Vp/Vs ratio) is highly sensitive to pore fluid type because shear waves are less affected by fluid content than P-waves.
Question 4: What is the purpose of applying a Normal Moveout (NMO) correction in seismic processing?
- To align reflections from the same subsurface point recorded at different offsets (Correct answer)
- To remove multiples caused by water-bottom reflections
- To correct for variations in surface elevation along the seismic line
- To convert time-domain data to depth-domain data
Correct answer: To align reflections from the same subsurface point recorded at different offsets
NMO correction removes the hyperbolic moveout effect so that reflections from the same subsurface point at different source-receiver offsets can be stacked coherently.
Question 5: A geologist observes high-amplitude seismic anomalies (bright spots) in a gas-prone basin. Which scenario would cause a FALSE bright spot?
- A tight carbonate with high acoustic impedance overlying a low-impedance shale (Correct answer)
- Gas-saturated sandstone with low impedance beneath a shale
- Coal seams within a clastic sequence
- Volcanic sills intruded into sedimentary rock
Correct answer: A tight carbonate with high acoustic impedance overlying a low-impedance shale
A hard kick from high-impedance carbonate over low-impedance shale produces a strong reflection that mimics a bright spot but contains no hydrocarbons.
Question 6: What does the term 'velocity pull-up' describe in seismic interpretation?
- An apparent structural high beneath a high-velocity body like a carbonate or salt (Correct answer)
- A reduction in seismic velocity due to overpressure
- The increase in velocity with depth in normally compacted shales
- Correction of velocity errors introduced during NMO
Correct answer: An apparent structural high beneath a high-velocity body like a carbonate or salt
Velocity pull-up is an artifact where reflectors beneath a high-velocity body appear structurally higher than they actually are because travel times are shortened.
Question 7: In the context of seismic facies analysis, what does 'chaotic' reflection pattern suggest?
- Mass transport deposits, slumps, or highly deformed sediments (Correct answer)
- Well-bedded, laterally continuous deep-water turbidites
- Fluvial channel fill with high lateral continuity
- Carbonate platform interior with uniform deposition
Correct answer: Mass transport deposits, slumps, or highly deformed sediments
Chaotic seismic facies lack internal organization and continuity, which is characteristic of mass transport complexes, slumps, or deformed sedimentary packages.
What does a flat spot on a seismic section typically indicate?