http://www.loc.gov/mods/v3 http://www.loc.gov/standards/mods/v3/mods-3-2.xsd
Rock Quality, Seismic Velocity, Attenuation and Anisotropy
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.
Part, Part I -- chapter 1 Shallow seismic refraction, some basic theory, and the importance of rock type -- chapter 2 Environmental effects on velocity -- chapter 3 Effects of anisotropy on Vp -- chapter 4 Cross-hole velocity and cross-hole velocity tomography -- chapter 5 Relationships between rock quality, depth and seismic velocity -- chapter 6 Deformation moduli and seismic velocities -- chapter 7 Excavation disturbed zones and their seismic properties -- chapter 8 Seismic measurements for tunnelling -- chapter 9 Relationships between Vp, Lugeon value, permeability and grouting in jointed rock -- part, Part II -- chapter 10 Seismic quality Q and attenuation at many scales -- chapter 11 Velocity structure of the earth's crust -- chapter 12 Rock stress, pore pressure, borehole stability and sonic logging -- chapter 13 Rock physics at laboratory scale -- chapter 14 P-waves for characterising fractured reservoirs -- chapter 15 Shear wave splitting in fractured reservoirs and resulting from earthquakes -- chapter 16 Joint stiffness and compliance and the joint shearing mechanism -- chapter 17 Conclusions.