Seismic Wave & Imaging (September 2016)
-
P-wave cannot pass through gaseous media.
-
True
-
False
-
QUIZ for QAB 3013: Seismic Wave & Imaging (September 2016 Semester)
Instruction to the students:
1. There are 11 multiple choice questions, 9 true / false questions.
2. Answer ALL the questions
3. Time given for this quiz is 25 minutes
4. No time extension will be allowed.
Good luck!
Quiz Preview
- 2.
Fresnel zone is a function of depth only.
-
True
-
False
Correct Answer
A. FalseExplanation
The given statement, "Fresnel zone is a function of depth only," is incorrect. The Fresnel zone is a concept used in wireless communication to determine the quality of a signal between a transmitter and receiver. It is not solely dependent on depth but also influenced by other factors such as distance, frequency, and obstacles in the signal path. Therefore, the correct answer is false.Rate this question:
-
- 3.
Reflection coefficient as a function of angle for a plane wave impinging on a plane reflector obeys Zoeppritz equations.
-
True
-
False
Correct Answer
A. TrueExplanation
The Zoeppritz equations are a set of mathematical equations that describe the reflection and transmission of seismic waves at an interface between two different rock layers. These equations are commonly used in geophysics to model the behavior of seismic waves and determine the reflection coefficient, which is a measure of the ratio of the amplitude of the reflected wave to the incident wave. Therefore, it is correct to say that the reflection coefficient as a function of angle for a plane wave impinging on a plane reflector obeys Zoeppritz equations.Rate this question:
-
- 4.
Rayleigh wave has velocity close to P-wave.
-
True
-
False
Correct Answer
A. FalseExplanation
Rayleigh waves, also known as ground roll, are a type of surface wave that travels along the surface of the Earth. They are slower than P-waves and have a velocity close to that of S-waves. Therefore, the given statement that Rayleigh waves have a velocity close to P-waves is incorrect.Rate this question:
-
- 5.
What is the TRUE concept of a wave?
-
Wave move in plane and only able to travel in a straight line.
-
Wave can be reflected, refracted, diffracted and transmitted.
-
Wave can’t be attenuated by any factor.
-
The wave movement is a process of heat transfer.
Correct Answer
A. Wave can be reflected, refracted, diffracted and transmitted.Explanation
A wave is a disturbance that transfers energy from one place to another without transferring matter. It can travel in different directions and can be reflected, refracted, diffracted, and transmitted. This means that waves can bounce off surfaces, change direction when passing through different mediums, spread out when passing through an opening, and continue propagating through a medium. Waves can be attenuated by factors such as absorption, scattering, or interference, so the statement that waves can't be attenuated by any factor is incorrect. The movement of waves is not directly related to heat transfer, as waves can transfer different forms of energy, not just heat.Rate this question:
-
- 6.
The following are the information can be obtained from a seismic trace EXCEPT:
-
Wavenumber.
-
Bulk Modulus.
-
Velocity.
-
Frequency.
Correct Answer
A. Bulk Modulus.Explanation
A seismic trace is a graphical representation of seismic waves recorded during seismic exploration. It provides information about various properties of the subsurface, such as velocity, frequency, and wavenumber. However, the bulk modulus is not directly obtained from a seismic trace. The bulk modulus is a measure of a material's resistance to compression and is typically determined through laboratory tests or other geophysical methods. Therefore, the correct answer is Bulk Modulus.Rate this question:
-
- 7.
Energy absorption occurs when the wave propagate through fast velocity zone.
-
True
-
False
Correct Answer
A. FalseExplanation
Energy absorption does not occur when the wave propagates through a fast velocity zone. In fact, energy absorption typically occurs when waves encounter zones of low velocity or high attenuation, where the energy of the wave is dissipated or absorbed. Therefore, the statement is false.Rate this question:
-
- 8.
Summing the energy along the diffraction hyperbola is a type of:
-
FK migration.
-
Kirchhoff migration.
-
Downward continuation migration.
-
Geometrical migration.
Correct Answer
A. Kirchhoff migration.Explanation
Summing the energy along the diffraction hyperbola refers to a technique called Kirchhoff migration. This migration method is used in seismic data processing to enhance the quality and resolution of subsurface images. It involves summing the energy contributions from different points on the diffraction hyperbola, which helps in accurately locating and imaging subsurface reflectors. Kirchhoff migration is a widely used technique in the oil and gas industry for interpreting seismic data and improving the understanding of subsurface structures.Rate this question:
-
- 9.
Which of the following sequence indicate the correct velocity sequence (from fastest to slowest) ?
-
Scholte wave --> Swave --> Rayleigh wave --> Love wave.
-
Pwave --> Swave --> Rayleigh wave --> Love wave .
-
Pwave --> Love wave --> Rayleigh wave --> Swave.
-
Pwave --> Stoneley wave --> Swave --> Scholte wave.
Correct Answer
A. Pwave --> Swave --> Rayleigh wave --> Love wave .Explanation
The correct answer is Pwave --> Swave --> Rayleigh wave --> Love wave. This sequence indicates the correct velocity sequence from fastest to slowest. Pwaves are primary waves that travel the fastest through the Earth's interior. Swaves are secondary waves that travel slower than Pwaves. Rayleigh waves are surface waves that move slower than both Pwaves and Swaves. Love waves are also surface waves but they have the slowest velocity among the four waves listed.Rate this question:
-
- 10.
Why do we need seismic migration / imaging?
-
Removing the effect of noise and multiples from the seismic data.
-
Enhancing velocity information of subsurface.
-
Correct apparent reflector position in preprocessing seismic data.
-
As a connector to GeologyGeophysics sequence (G&G Link).
Correct Answer
A. Correct apparent reflector position in preprocessing seismic data.Explanation
Seismic migration/imaging is necessary to correct the apparent reflector position in preprocessing seismic data. During seismic data acquisition, the recorded signals can be distorted due to various factors such as the velocity variations in the subsurface, the presence of noise, and the occurrence of multiple reflections. Seismic migration helps in accurately determining the position of the reflectors by accounting for these distortions and providing a clearer image of the subsurface. This is crucial for geological interpretation and exploration purposes.Rate this question:
-
- 11.
Diffraction curves are wider as depth increases.
-
True
-
False
Correct Answer
A. TrueExplanation
As depth increases, the diffraction curves become wider. This is because diffraction is the bending of waves around obstacles or through openings, and the wider the opening or obstacle, the more the waves spread out. Therefore, as the depth increases, the waves have more space to spread out, resulting in wider diffraction curves.Rate this question:
-
- 12.
An unmigrated dipping reflector has a 25 degree dip measured from the flat surface. Calculate the migrated reflector dipping angle.
-
22.91 degree
-
25.91 degree
-
27.79 degree
-
37.79 degree
Correct Answer
A. 27.79 degree -
- 13.
When a Pwave strikes an interface, the energy will be partitioned into the following waveEXCEPT:
-
Reflected Shear wave.
-
Transmitted Shear wave.
-
Reflected Surface wave.
-
Reflected Pressure wave.
Correct Answer
A. Reflected Surface wave.Explanation
When a P-wave strikes an interface, it can be either reflected or transmitted as different types of waves. The energy of the P-wave can be partitioned into reflected shear waves, transmitted shear waves, and reflected pressure waves. However, it does not result in the generation of a reflected surface wave. Surface waves are typically generated by the interaction of S-waves with the Earth's surface, not P-waves. Therefore, the correct answer is "Reflected Surface wave."Rate this question:
-
- 14.
The following is principle of Huygens’ Principle EXCEPT:
-
Every point is the source of a secondary wave front.
-
These secondary wave front can propagate upward or downward.
-
Amplitude & phase in secondary wave front is same as the primary wave front.
-
The superposition of these secondary wave front will create a new wave front.
Correct Answer
A. Amplitude & phase in secondary wave front is same as the primary wave front.Explanation
Huygens' principle states that every point on a wavefront acts as a source of secondary wavelets, which propagate in all directions. These secondary wavelets have the same amplitude and phase as the primary wavefront. The superposition of these secondary wavelets creates a new wavefront. Therefore, the correct answer is that the amplitude and phase in the secondary wavefront are the same as the primary wavefront.Rate this question:
-
- 15.
Diffraction hyperbola for a constant velocity is:
-
Same irrespective of depth.
-
Narrower as depth increase.
-
Broader as depth increase.
-
Shorter as depth increase.
Correct Answer
A. Broader as depth increase.Explanation
The diffraction hyperbola refers to the pattern of diffraction caused by a constant velocity wavefront encountering an obstacle. As the depth increases, the diffraction hyperbola becomes broader. This is because as the wavefront encounters the obstacle at greater depths, the diffracted waves spread out more, resulting in a broader pattern. Therefore, the correct answer is "Broader as depth increases."Rate this question:
-
- 16.
Which one of the following statements regarding real geology, time migration & depth migration is TRUE:
-
Time section migration is equivalent with depth migration.
-
There is discrepancies of time and depth migration.
-
Time migration requires a velocity model for imaging.
-
Time migration better image the points position compare to depth migration.
Correct Answer
A. There is discrepancies of time and depth migration.Explanation
The statement "There is discrepancies of time and depth migration" is true. Time migration and depth migration are two different methods used in geology for imaging subsurface structures. Time migration involves correcting seismic data for the effects of the velocity model, while depth migration directly images the subsurface based on the true depth. These two methods can produce different results and there can be discrepancies between them.Rate this question:
-
- 17.
Acoustic wave can be derived from Newton 1st Law and Hooke's Law.
-
True
-
False
Correct Answer
A. FalseExplanation
The statement is false because acoustic waves cannot be directly derived from Newton's First Law and Hooke's Law. Newton's First Law states that an object at rest will stay at rest unless acted upon by an external force, while Hooke's Law states that the force needed to extend or compress a spring is directly proportional to the distance it is stretched or compressed. These laws do not specifically describe the generation or propagation of sound waves, which require the presence of a medium such as air or water.Rate this question:
-
- 18.
A diffraction response for a homogeneous single velocity media is:
-
NonHyperbolic.
-
Amplitude decays exponentially from apex.
-
Phase is asymmetrical.
-
Frequency attenuated with depth.
Correct Answer
A. Amplitude decays exponentially from apex.Explanation
The given statement states that the diffraction response for a homogeneous single velocity media is that the amplitude decays exponentially from the apex. This means that as the diffraction wave propagates through the medium, the amplitude of the wave decreases exponentially as it moves away from the source or apex. This is a characteristic behavior of diffraction in such a medium.Rate this question:
-
- 19.
Shear wave cannot pass through saturated rock.
-
True
-
False
Correct Answer
A. FalseExplanation
Shear waves can actually pass through saturated rock. In fact, shear waves travel slower in saturated rock compared to dry rock due to the presence of water. This is because the water molecules in the rock impede the movement of shear waves, causing them to slow down. Therefore, the correct answer is False.Rate this question:
-
- 20.
Lowering full fold data may affect the resolution of the seismic data.
-
True
-
False
Correct Answer
A. FalseExplanation
Lowering the fold data refers to reducing the number of times a particular point in the subsurface is sampled during seismic data acquisition. This can be done to save costs or improve efficiency. However, it is important to note that lowering the fold data can indeed affect the resolution of the seismic data. Higher fold data provides more redundant information, which helps to reduce noise and improve the signal-to-noise ratio, leading to better resolution. Therefore, reducing the fold data can result in a decrease in the quality and resolution of the seismic data.Rate this question:
-
Quiz Review Timeline (Updated): Mar 18, 2023 +
Our quizzes are rigorously reviewed, monitored and continuously updated by our expert board to maintain accuracy, relevance, and timeliness.
-
Current Version
-
Mar 18, 2023Quiz Edited by
ProProfs Editorial Team -
Dec 16, 2016Quiz Created by
Luluan
Back to top