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影響因子(影響力)




書目名稱Experimental Techniques in Mineral and Rock Physics影響因子(影響力)學科排名




書目名稱Experimental Techniques in Mineral and Rock Physics網絡公開度




書目名稱Experimental Techniques in Mineral and Rock Physics網絡公開度學科排名




書目名稱Experimental Techniques in Mineral and Rock Physics被引頻次




書目名稱Experimental Techniques in Mineral and Rock Physics被引頻次學科排名




書目名稱Experimental Techniques in Mineral and Rock Physics年度引用




書目名稱Experimental Techniques in Mineral and Rock Physics年度引用學科排名




書目名稱Experimental Techniques in Mineral and Rock Physics讀者反饋




書目名稱Experimental Techniques in Mineral and Rock Physics讀者反饋學科排名

perpetual

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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ETHER

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

ETHER

perpetual

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

潰爛

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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