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Titlebook: Experimental Techniques in Mineral and Rock Physics; The Schreiber Volume Robert C. Liebermann,Carl H. Sondergeld Book 1994 Springer Basel

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書目名稱Experimental Techniques in Mineral and Rock Physics
副標題The Schreiber Volume
編輯Robert C. Liebermann,Carl H. Sondergeld
視頻videohttp://file.papertrans.cn/319/318940/318940.mp4
叢書名稱Pageoph Topical Volumes
圖書封面Titlebook: Experimental Techniques in Mineral and Rock Physics; The Schreiber Volume Robert C. Liebermann,Carl H. Sondergeld Book 1994 Springer Basel
描述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
出版日期Book 1994
關(guān)鍵詞geophysics; mineral; sediment; sedimentary rock; seismic
版次1
doihttps://doi.org/10.1007/978-3-0348-5108-4
isbn_softcover978-3-7643-5028-4
isbn_ebook978-3-0348-5108-4Series ISSN 2504-3625 Series E-ISSN 2504-3633
issn_series 2504-3625
copyrightSpringer Basel AG 1994
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Reflections on the Career of Edward Schreiber on his way to Queens College, an institution with which he had had a long and valuable association. Ed was born in Brooklyn in 1930. He attended the New York State College of Ceramic Engineering at Alfred University where he received his B.S. degree Magna Cum Laude in 1956 and his Ph.D. degree in 1
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Experimental Simulation of Plagioclase Diagenesis at , Conditions of 3.5 km Burial Depthon in feldspathic siliciclastic sediments. The diagenetic behavior of granular aggregates of plagioclase feldspar and quartz has been investigated by experimentation performed in a Bridgeman-type pressure vessel. The experiments, each of two weeks duration, simulated pressure-temperature conditions
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Controls on Sonic Velocity in Carbonatesg and pore-fluid pressures. The lithologies of the samples range from unconsolidated carbonate mud to completely lithified limestones. The velocity measurements enable us to relate velocity variations in carbonates to factors such as mineralogy, porosity, pore types and density and to quantify the v
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A New Ultrasonic Interferometer for the Determination of Equation of State Parameters of Sub-millime1.5 GHz. The high frequency and associated small wavelengths together with the large bandwidth make it possible to measure travel times in samples with thicknesses of several microns and allow for unprecedented accuracy in bond corrections. An absolute accuracy of 1 part in 10. in travel time measur
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Performance of the Complete Travel-time Equation of State at Simultaneous High Pressure and Temperatasonic experimental data under simultaneous high pressure and high temperature without introducing any assumption, as long as the density, or thermal expansivity, and heat capacity are also available as functions of temperature at zero pressure. The performance of the CT-EOS was examined by using sy
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