The Polarization Method of Seismic Exploration
variegated seismological conditions has been accumulated. The method has been developed further in two main directions: - the perfection of the techniques and equipment of three-component field studies incorporating a continuous control of the identity of equipment both in deep boreholes and on the...
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| Format: | eBook |
| Language: | English |
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Dordrecht
Springer Netherlands
1984, 1984
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| Edition: | 1st ed. 1984 |
| Series: | Solid Earth Sciences Library
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| Subjects: | |
| Online Access: | |
| Collection: | Springer Book Archives -2004 - Collection details see MPG.ReNa |
Table of Contents:
- 1: physical and geological foundations of the Polarization method
- Physical Premises for Increasing the Efficiency of Seismic Methods Used in the Study of Media with Complex Structures
- General Information on the Polarization of Seismic Waves
- Brief Review of Papers Dealing with the Study of Polarization of Seismic Waves
- Selected Results from the Theory of Harmonic Oscillations
- Stereographic Projections
- Controlled Directional Reception Based on Displacement Directions (CDR—I)
- Polarization Filtering
- Methods of Representing Trajectories of Particle Motion
- 2: Instrumentation For Three-Component Observations Using The Polarization Method
- Three-Component Sets
- Making Multi-Component Polar Seismograms
- Instrumentation and Methods for Producing Oriented Records
- Fixed- and Tracking-Components Block
- Equipment for Three-Component Observations and Data Processing Used in Seismic Prospecting
- 3: Polar Correlation of Seismic Waves
- Use of PPC in Seismic Prospecting for Oil
- Use of PPC in Establishing Continuity for Converted PS Waves Resulting from Distant Earthquakes
- 6: study of media on the basis of seismic wave Polarization
- Effect of Low-Velocity Layers (LVL) on Wave Polarization
- Study of Particle Displacement in a Vertical Plane
- Location of the Boundary Position from Transmitted Waves in VSP
- Locating the Position of the Boundary from Converted Transmitted Waves in Surface Observations
- Locating the Position of a Refracting Boundary from the Polarization of Compressionl Waves
- Conclusion
- References
- Appendix - Glossary
- Index of Subjects
- Index of Names
- Derivation of Equations for Line-Ups and Amplitudes of Elliptically-Polarized Oscillations
- Analysis of Equations for Line-Ups and Amplitudes of Linearly-Polarized Waves
- Analysis of Equations for Line-Ups and Amplitudes of Elliptically-Polarized Waves
- Plotting Polar Seismograms
- Determination of Parameters of Linearly-Polarized Oscillations
- Determination of Parameters of Elliptically- and Multiply-Polarized Waves
- 4: Application of Seismic-Wave Polar Correlation
- Polarization of Explosion-Induced Direct P and S Waves
- Polarization of Direct Shear and Other Waves Induced by Weak Local Earthquakes
- Polar Correlation of Transmitted Converted Waves Induced by Distant Earthquakes
- Use of Polar Correlation in Studies Concerned with the Effect of Observation Conditions on the Shape of Wave Records
- 5:polarization-position correlation (ppc) of Seismic waves
- An Outline of PPC
- Practical Procedure for PPC
- Use of PPC in Seismic Prospecting for Ores