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Modelling of transient flow and pressure behaviour in multilayer stratified reservoirsAl-Gheithy, Ali Amor January 1993 (has links)
No description available.
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Empirical modelling of Canadian petroleum exploration activityDesbarats, C. M. January 1987 (has links)
No description available.
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Phenols in petroleum systemsLucach, Sandra Ortega January 2003 (has links)
No description available.
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Development and application of inductively coupled plasma-mass spectrometry for the analysis of metals in sedimentary organic matterOlsen, Samuel Dagfinn January 1996 (has links)
No description available.
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Overpressure in the Central North SeaDarby, David January 1995 (has links)
No description available.
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The biotreatment of spent caustic wasteFerguson, A. S. January 2001 (has links)
No description available.
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Reservoir diagenesis in the Junggar Basin, northwest ChinaTang, Zhaohui January 1994 (has links)
No description available.
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Computerised kick detection using surface measurementsWilliams, Peter R. January 1997 (has links)
No description available.
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Geochemical modeling and hydrothermal experiments used to constrain the conditions of illite diagenesis in sedimentary basinsMurphy, Michael Joseph 11 February 2017 (has links)
<p> Two hydrothermal experiments were performed using sandstone core material from the Norwegian North Sea with synthetic brines reacted at approximately 150°C and 450 bars, temperature and pressure calculated to simulate a depth of burial of approximately 4 km. The results of the experiments were analyzed with geochemical modeling and with chemical and petrographic analyses. Geochemical modeling with several computer programs indicated that the experimental fluid was undersaturated with respect to K-feldspar, kaolinite, and illite, but supersaturated with respect to muscovite. Chemical analysis with inductively-coupled plasma mass spectrometry indicated that the fluid reached saturation with respect to K-feldspar. Petrographic analysis with scanning electron microscopy and energy-dispersive scanning indicated that changes took place over the course of the experiments in both the clay and non-clay mineral fractions, and this result was verified by X-ray diffraction analysis that indicated dissolution of both K-feldspar and illite and formation of muscovite. These converging lines of evidence indicate that significant changes took place in the clay mineral fraction of the experimental sandstone core material, reacted at realistic basin temperature, pressure and geochemical conditions, over the course of several weeks.</p>
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An application of rational choice theory to petroleum policies in Canada, Britain, and NorwayEdwards, Miriam Ruth Germaine January 1988 (has links)
No description available.
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