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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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https://doi.org/10.1007/978-3-7091-8925-2g 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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https://doi.org/10.1007/978-3-658-07889-8described as a qualitative application of thermal analysis. Discontinuities in temperature, laser power, visible thermal radiation, or in their derivatives as functions of time can be associated with the enthalpy of phase transitions (such as melting) or with changes in material properties (such as
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Studies in Computational Intelligenceadiation. The first method employs a white X-ray beam using energy dispersive X-ray diffraction. The incident X-ray beam is parallel to the load axis and the diffraction pattern is recorded at a low two-theta angle. Using powder diffraction patterns of polycrystalline gold, we measured the elastic s
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