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Principles of Onshore 3-D Seismic Design

GC9705

Principles of Onshore 3-D Seismic Design, by B. A. Hardage. 23 p., 13 figs., 1997. ISSN: 0082-3309. Print Version.

For a downloadable, digital version: GC9705D.

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GC9705. Principles of Onshore 3-D Seismic Design, by B. A. Hardage. 23 p., 13 figs., 1997. ISSN: 0082-3309. Print.


To order this publication as a downloadable PDF, please order GC9705D.


ABSTRACT
The basic geometry of an onshore three-dimensional (3-D) seismic recording grid is based on five parameters: source-station spacing, receiver-station spacing, source-line spacing. receiver-line spacing, and recording swath size. At each onshore prospect considered for 3-D seismic imaging, these key design parameters can be specified by answering four simple questions: 1. What is the narrowest lateral dimension of the geologic targets that are to be imaged? 2. What is the depth of the shallowest target that must be imaged? 3. What is the depth of the deepest target that must be imaged? 4. What stacking fold is required to create an acceptable image at the depth of the principal target? The first three questions can be answered once the geology of the prospect is reasonably well known. The fourth question can be answered by (1) examining two-dimensional (2-D) seismic profiles that traverse the prospect area to estimate reflection signal quality, (2) examining 3-D seismic data recorded near the prospect, or (3) making a best guess, which is a risky and less desirable approach. Once these four questions are answered, the methodology described herein allows many onshore 3-D seismic recording grids to be designed without having to use complex computations or commercial design software. Some of the more technical aspects of 3-D seismic design, such as ensuring that there is a proper azimuth distribution of source-receiver offsets or creating a continuous numerical range of source-receiver offsets across the entire acquisition grid, are not considered in this simple treatise on first principles. The intent is to provide a procedure that allows nongeophysicists to plan simple 3-D surveys and to recognize flaws in proposed 3-D programs. This design procedure should be helpful to people who wish to verify the imaging capabilities of a particular 3-D seismic design but who do not access to, or wish to use, extensive computational resources.

 

Keywords: recording swath, stacking bin, stacking fold, three-dimensional design, three-dimensional seismic


CONTENTS

Abstract

Introduction

Key Design Parameters

Cost Rule: Minimize the Number of Source Stations

Narrowest Target to Image and Stacking Bin Size

Source-Station and Receiver-Station Spacings Depth of Shallowest Target and Its Implications: Source-Line and Receiver-Line Spacings

Depth of Primary (or Deepest) Target and Its Implication: Size of the Recording Swath

Stacking Fold Variation with Depth

3-D Stacking Fold

In-line Stacking Fold

Cross-line Stacking Fold

Example Calculation of 3-D Stacking Fold

Final Design Step: Comparing the Design Fold and the Desired Fold

The Even-Integer Rule

Summary

Acknowledgments

References

Epilogue



Figures

1. Sequence of planning steps that mill be followed to create an onshore 3-D seismic acquisition geometry

2. Oblique view of a horizontal grid of 3-D stacking bins

3. Example of the narowest feature that needs to be seen in the 3-D image

4. Section view of the Earth layering that is to be imaged.

5. An example of so~irce/receiver-lines pacings designed to image a shallow target at a depth of ZI

6. Recording swath designed to image a deep target at a depth Z

7. Vertical variation in stacking fold

8. Effect of number of active receivers on in-line stacking fold

9. Effect of source-station spacing on in-line stacking fold

10. Concept of cross-line stacking fold

11. The even-integer rule for onshore 3-D seismic design

12. Comparison of two 3-D recording swaths

13. Comparison of softtifare-generated stacking folds created by swath




Citation
Hardage, B. A., 1997, Principles of Onshore 3-D Seismic Design: The University of Texas at Austin, Bureau of Economic Geology, Geological Circular 97-5, 23 p.

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