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Seismic measurements take many forms, and appear to have a universal role in the Earth Sciences. They are the means for most easily and economically interpreting what lies beneath the visible surface. There are huge economic rewards and losses to be made when interpreting the shallow crust or subsurface more, or less accurately, as the case may be.
Seismic measurements take many forms, and appear to have a universal role in the Earth Sciences. They are the means for most easily and economically interpreting what lies beneath the visible surface. There are huge economic rewards and losses to be made when interpreting the shallow crust or subsurface more, or less accurately, as the case may be.
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Autorenporträt
Nick Barton
Inhaltsangabe
The Multidisciplinary Scope of Seismic and Rock Quality. Revealing Hidden Rock Conditions. Some Basic Principles of P, S and Q. Q and Q XVII Limitations of Refraction Seismic Bring Tomographic Solutions. Part 1: 1. Shallow Seismic Refraction, some Basic Theory, and the Importance of Rock Type 2. Environmental Effects on Velocity 3. Effects of Anisotropy on Vp 4. Cross-Hole Velocity and Cross-Hole Velocity Tomography 5. Relationships between Rock Quality, Depth and Seismic Velocity 6. Deformation Moduli and Seismic Velocities 7. Excavation Disturbed Zones and their Seismic Properties 8. Seismic Measurements for Tunnelling 9. Relationships between Vp, Lugeon Value, Permeability and Grouting in Jointed Rock Part 2: 10. Seismic Quality Q and Attenuation at Many Scales 11. Velocity Structure of the Earth's Crust 12. Rock Stress, Pore Pressure, Borehole Stability and Sonic Logging 13. Rock Physics at Laboratory Scale 14. P-Waves for Characterising Fractured Reservoirs 15. Shear Wave Splitting in Fractured Reservoirs and Resulting from Earthquakes 16. Joint Stiffness and Compliance and the Joint Shearing Mechanism 17. Conclusions Appendix A: The Qrock Parameter Ratings
The Multidisciplinary Scope of Seismic and Rock Quality. Revealing Hidden Rock Conditions. Some Basic Principles of P, S and Q. Q and Q XVII Limitations of Refraction Seismic Bring Tomographic Solutions. Part 1: 1. Shallow Seismic Refraction, some Basic Theory, and the Importance of Rock Type 2. Environmental Effects on Velocity 3. Effects of Anisotropy on Vp 4. Cross-Hole Velocity and Cross-Hole Velocity Tomography 5. Relationships between Rock Quality, Depth and Seismic Velocity 6. Deformation Moduli and Seismic Velocities 7. Excavation Disturbed Zones and their Seismic Properties 8. Seismic Measurements for Tunnelling 9. Relationships between Vp, Lugeon Value, Permeability and Grouting in Jointed Rock Part 2: 10. Seismic Quality Q and Attenuation at Many Scales 11. Velocity Structure of the Earth's Crust 12. Rock Stress, Pore Pressure, Borehole Stability and Sonic Logging 13. Rock Physics at Laboratory Scale 14. P-Waves for Characterising Fractured Reservoirs 15. Shear Wave Splitting in Fractured Reservoirs and Resulting from Earthquakes 16. Joint Stiffness and Compliance and the Joint Shearing Mechanism 17. Conclusions Appendix A: The Qrock Parameter Ratings
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