Instructions: Choose the best answer for each question.
1. What is the primary goal of kriging in seismic exploration? a) To identify the exact location of oil and gas reservoirs. b) To estimate unknown seismic values at unsampled locations. c) To create a 3D model of the Earth's subsurface. d) To analyze the frequency content of seismic data.
b) To estimate unknown seismic values at unsampled locations.
2. What does the variogram represent in kriging? a) The average value of seismic data. b) The spatial correlation between data points. c) The geological structure of the subsurface. d) The signal-to-noise ratio in seismic data.
b) The spatial correlation between data points.
3. How does kriging calculate the estimated value at an unsampled location? a) By averaging all known values. b) By using a predefined interpolation formula. c) By weighting known values based on their spatial correlation. d) By applying a Fourier transform to the data.
c) By weighting known values based on their spatial correlation.
4. Which of the following is NOT a key application of kriging in seismic exploration? a) Seismic attribute mapping. b) Seismic inversion. c) Seismic data denoising. d) Seismic velocity analysis.
d) Seismic velocity analysis.
5. What is a major advantage of using kriging in seismic exploration? a) It provides a complete and accurate picture of the subsurface. b) It eliminates the need for seismic data acquisition. c) It offers a statistically sound framework for quantifying uncertainty. d) It is computationally inexpensive and easy to implement.
c) It offers a statistically sound framework for quantifying uncertainty.
Scenario: You have collected seismic data from a region of interest. You have measured a specific seismic attribute (e.g., amplitude) at several locations within the area.
Task:
Exercise Correction:
A complete correction for this exercise would require specific software or online resources, as well as a dataset of known seismic attribute values. The steps involved in the exercise would be as follows:
This exercise would demonstrate the application of kriging in generating a detailed map of a seismic attribute, which can be further analyzed to gain insights into the subsurface geology.
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