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The Global ETD Search service is a free service for researchers
to find electronic theses and dissertations. This service is
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Networked Digital Library of Theses and Dissertations.
Our metadata is collected from universities around the world. If you manage a university/consortium/country archive and want to be added, details can be found on the NDLTD website.
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Showing 71 to 80 of 325 (0.027 seconds)Spelling suggestions: "subject:"argon"" "subject:"ergon""
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Etude des hétérogénéités morphologiques et énergétiques superficielles des kaolinites par AFM et adsorption de gazSayed Hassan, Malak Villieras, Frédéric. January 2005 (has links) (PDF)
Thèse de doctorat : Géosciences : Vandoeuvre-les-Nancy, INPL : 2005. / Titre provenant de l'écran-titre. Bibliogr.
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| 72 |
The equation of state of frozen neon, argon, krypton, and xenon ...Kane, Conrad Gabriel. January 1939 (has links)
Thesis (Ph. D.)--Catholic University of America, 1939. / Cover title. From Journal of chemical physics, v. 7, Aug. 1939.
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| 73 |
Simulation of structure, dynamics and electron diffraction patterns of heterogeneous clusters Arm(N₂)n /Jinasena W. H., January 2002 (has links)
Thesis (Ph. D.) in Chemistry--University of Maine, 2002. / Includes vita. Includes bibliographical references (leaves 157-169).
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| 74 |
Electrical breakdown studies of partial pressure argon under Khz range pulse voltagesLipham, Mark Lawrence. Kirkici, Hulya. January 2010 (has links)
Thesis--Auburn University, 2010. / Abstract. Includes bibliographic references (p.55-56).
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| 75 |
THE THERMODYNAMICS OF THE ADSORPTION OF ARGON ON ANATASEGlossman, Norton, 1935- January 1964 (has links)
No description available.
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| 76 |
Many body interactions : part one, Interactions between solute molecules in liquid argon ; part two, The interaction between krypton and the (1, 1, 0) face of copper single crystalsParrott, Stephen Laurent 08 1900 (has links)
No description available.
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| 77 |
Phase equilibria in the argon-helium and argon-hydrogen systemsMullins, Joseph Chester 05 1900 (has links)
No description available.
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| 78 |
Argon-Assisted Glancing Angle DepositionSorge, Jason B Unknown Date
No description available.
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| 79 |
Improvements to the resolution and efficiency of the DEAP-3600 dark matter detector and their effects on background studiesOlsen, Kevin Sutherland Unknown Date
No description available.
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| 80 |
Magmatic and tectonic evolution of Southern Tibet and the HimalayaWilliams, Helen Myfanwy January 2000 (has links)
The Himalaya-Tibetan orogen has become the paradigm for continental collision and is central to deciphering continental tectonics. Neogene extension in the orogen is not predicted by plate tectonic theory, and its significance is widely debated. In the Himalaya, north-south extension is restricted to the Southern Tibetan Detachment System (STDS), which juxtaposes the High Himalayan Crystalline Series (HHCS) against the Tibetan Sedimentary Series (TSS). <sup>40</sup>Ar-<sup>39</sup>Ar ages from HHCS and TSS of the Garhwal Himalaya indicate that STDS movement initiated between 17.3 ± 0.4 to 24.3 ± 1.6 Ma (2σ), synchronous with Main Central Thrust (MCT) movement. One-dimensional thermal modelling suggests that the STDS is a reactivated thrust, implying a fundamental change in Himalayan tectonics in the early Miocene. The onset of east-west extension in southern Tibet is constrained by north-south trending shoshonitic dykes to be 13.3 ± 0.8-18.3 ± 2.7 Ma. Trace-element modelling indicates that the shoshonitic dykes and associated lavas in southern and northern Tibet were derived by ≤2% melting of enriched sub-continental lithospheric mantle (SCLM) at 65-85km. The northern and southern shoshonites have distinctive isotopic (εNd<sub>(i)</sub>, north, -5.5 to-10.3; south -8.8 to - 18.1) and major element signatures that relate to distinct SCLM sources corresponding to the tectonically accreted terranes of the plateau. The trace-element compositions of these sources, determined by inverse modelling, suggest subduction-related metasomatism. <sup>40</sup>Ar- <sup>39</sup>Ar dating of xenocrystic phlogopites indicates metasomatism of the southern SCLM occurred at 62±2 Ma, synchronous with collision. These data link Neogene extension to a thermally perturbed lithosphere. SCLM thinning following slab detachment explains magmatism, extension and uplift in southern Tibet. Episodic convective removal of the SCLM is proposed for northern Tibet. In view of these models, initiation of extension at 18.3±1.6 Ma in southern Tibet places a minimum constraint on plateau uplift. This overlaps with STDS and MCT movement, implying that changes in Himalayan tectonics are controlled by plateau uplift.
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