Overview
- Editors:
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Robert C. Liebermann
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Center for High Pressure Research, Department of Earth and Space Sciences, University at Stony Brook, Stony Brook, USA
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Carl H. Sondergeld
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Rock Properties, Theoretical Geophysical Research, Amoco Production Company Research Center, Tulsa, USA
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Table of contents (24 chapters)
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Introduction
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- Robert C. Liebermann, Carl H. Sondergeld
Pages 209-209
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Reflections on the Career of Edward Schreiber
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- Robert C. Liebermann, William A. Bassett
Pages 211-217
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Rocks and Rock Properties
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Front Matter
Pages 219-219
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- Stephen L. Karner, B. Charlotte Schreiber
Pages 221-247
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- Carl H. Sondergeld, Chandra S. Rai
Pages 249-268
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- Flavio S. Anselmetti, Gregor P. Eberli
Pages 287-323
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Acoustic Studies of the Elasticity and Equation of State of Minerals
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Front Matter
Pages 325-325
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- Orson L. Anderson, Donald G. Isaak
Pages 327-339
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- Hartmut A. Spetzler, Ganglin Chen, Scott Whitehead, Ivan C. Getting
Pages 341-377
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- Hartmut A. Spetzler, Akira Yoneda
Pages 379-392
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- Donald G. Isaak, Earl K. Graham, Jay D. Bass, Hong Wang
Pages 393-414
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- Hyunchae Cynn, Orson L. Anderson, Malcolm Nicol
Pages 415-444
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- Ian Jackson, M. S. Paterson
Pages 445-466
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- Gabriel D. Gwanmesia, Baosheng Li, Robert C. Liebermann
Pages 467-484
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Diamond-anvil Cell Experiments
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Front Matter
Pages 485-485
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- W. A. Bassett, A. H. Shen, M. Bucknum, I-Ming Chou
Pages 487-495
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- Jeffrey S. Sweeney, Dion L. Heinz
Pages 497-507
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About this book
Knowledge of the relation between sonic velocity in sediments and rock lithology is one of the keys to interpreting data from seismic sections or from acoustic logs of sedimentary sequences. Reliable correlations of rock velocity with other petrophysical parameters, such as porosity or density, are essential for calculating impedance models for synthetic seismic sections (BIDDLE et al. , 1992; CAMPBELL and STAFLEU, 1992) or identifying the origin of reflectivity on seismic lines (SELLAMI et al. , 1990; CHRISTENSEN and SZYMANSKI, 1991). Velocity is thus an important parameter for correlating lithological with geophysical data. Recent studies have increased our understanding of elastic rock properties in siliciclastic or shaly sediments. The causes for variations in velocity have been investigated for siliciclastic rocks (VERNIK and NUR, 1992), mixed carbonate siliciclastic sediments (CHRISTENSEN and SZYMANSKI, 1991), synthetic sand-clay mixtures (MARION et aI. , 1992) or claystones (JAPSEN, 1993). The concepts derived from these studies are however only partly applicable in pure carbonates. Carbon ates do not have large compositional variations that are, as is the case in the other sedimentary rocks, responsible for velocity contrasts. Pure carbonates are character ized by the lack of any clay or siliciclastic content, but are mostly produced and deposited on the top or on the slope of isolated or detached carbonate platforms, that have no hinterland as a source of terrigeneous material (WILSON, 1975; EBERLI, 1991).
Editors and Affiliations
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Center for High Pressure Research, Department of Earth and Space Sciences, University at Stony Brook, Stony Brook, USA
Robert C. Liebermann
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Rock Properties, Theoretical Geophysical Research, Amoco Production Company Research Center, Tulsa, USA
Carl H. Sondergeld