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Tot cieraet ende aensien deser stede : Arent van 's-Gravesande (ca. 1610-1666), architect en ingenieur /Steenmeijer, Guido. January 2005 (has links)
Texte remanié de: Proefschrift--Leiden--Universiteit, 2001. / Bibliogr. p. 332-342. Résumé en anglais et en allemand.
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92 |
Relating behavioral context to acoustic parameters of bottlenose dolphin (Tursiops truncatus) vocalizations /Thomas, Rebecca Elizabeth. January 1900 (has links)
Thesis (Ph. D.)--Joint Program in Oceanography (Massachusetts Institute of Technology, Dept. of Biology, and the Woods Hole Oceanographic Institution), 2001. / Includes bibliographical references.
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93 |
N.S. Leskovs Romanchronik "Die Klerisei." Von ihrer ursprünglichen Konzeption bis zur endgültigen GestaltungGollert, Ingeborg, January 1969 (has links)
Inaug.-Diss.--Freie Universität, Berlin. / Vita. Bibliography: p. 5-25.
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Menneske først Grundtvigs opgør med sig selv.Thaning, Kaj. January 1963 (has links)
Thesis--Copenhagen. / Summary in German. Includes bibliographical references.
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95 |
Die Struktur des Dramas bei T.S. EliotSchmidt, Gerd, January 1962 (has links)
Thesis--Freiburg i. Br. / Includes bibliographical references.
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96 |
Symbolische Landschaft bei T.S. Eliot Untersuchungen zu Entwicklung, Funktion und christlicher Tradition eines zentralen Motivs seines lyrischen Schaffens.Steinbach, Renate Schneider, January 1972 (has links)
Inaug.-Diss.--Philipps-Universität, Marburg. / Bibliography: p. 359-387.
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97 |
The Truman assassination attempt in the American consciousness /Smith, Kenneth R., January 2003 (has links)
Thesis (M.S.)--Central Connecticut State University, 2003. / Thesis advisor: Alfred Richard. In partial fulfillment of the requirements for the degree of Master of Science in History. Includes bibliographical references (leaves 97-99). Also available via the World Wide Web.
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Charles Peirce's empiricismBuchler, Justus, January 1939 (has links)
Thesis (Ph. D.)--Columbia University, 1939.
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99 |
A critical study of the Chinese translations of T.S. Eliot's early poetry, 1917-1920 /Chu, Siu-bing, Rita. January 1988 (has links)
Thesis (M. Phil.)--University of Hong Kong, 1988.
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Structure and genesis of the South Pennine orefieldQuirk, David Gordon January 1987 (has links)
Mineralisation in the South Pennine MVT orefield (225km2) has resulted from the combined effects of basement structure, stress history and basin evolution during the Carboniferous. NW-SE-trending Caledonian thrusts in the basement beneath North Derbyshire were reactivated as normal growth faults during limestone sedimentation in the Dinantian. on a regional scale, a major low-angle detachment, dipping NE away from St. George's Land (20km to the SW of North Derbyshire), controlled basin development as far as the Askern-Spital High (100km to the NE). The North Derbyshire shelf developed on the up-dip crest of a NE-tilted half-graben, in the hanging wall of this detachment, directly above the zone of mantle upwelling. A similar structure also evolved in the Rotherham area, some 40km to the NE, where, it is inferred, another orefield exists in the subsurface. In North Derbyshire, the end of the Dinantian was a period of uplift and erosion. In the NE part of the shelf, dextral wrench faults developed above ENE-WSW-trending basement fractures. At the start of the Namurian the direction of extension rotated to NW-SE and by the end of the Westphalian the limestone was buried to a depth of about 2km (~130°C) due to the combined effects of thermal sag and sediment compaction. Mineralisation began in the early Stephanian, associated with a period of N-S extension. Fractures in the limestone formed during earlier tectonic events began to dilate, thus allowing inflow of acidic F-Ba-Pb-zn-S-enriched fluid expelled from overlying Namurian shales. This was replenished by meteoric water migrating westwards down-dip from the uplifted Askern-Spital-Nocton-Grantham High. Ore deposition occurred within the limestone as a result of increasing pH, Ca 2+ and SO42 in the orefluid due to wallrock dissolution and fluid mixing. Mineralisation probably continues in the subsurface for some distance to the SE of the South Pennine orefield in shallow-water limestones with a similar structural aspect to those exposed in North Derbyshire.
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