Thesis (M.S.)--University of Tennessee, Knoxville, 2008. / Title from title page screen (viewed on Sept. 30, 2009). Thesis advisor: Steven N. Waller. Vita. Includes bibliographical references.

Thesis (M.A.)--Georgia State University, 2009. / Title from title page (Digital Archive@GSU, viewed July 16, 2010) Matthew Roudane, committee chair; Pearl McHaney, Wayne Erickson, committee members. Includes bibliographical references (p. 85-88).

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No description available.

East Tennessee State University formally became a college in 1925 with the institution changing its name to East Tennessee State Teachers College. It would subsequently gain accreditation in 1927. Included here is the East Tennessee State University portion of the Annual Report of the Tennessee Department of Education for the scholastic year ending June 30, 1925. Outlined in this report is the general description of events that happened over the course of that year including details surrounding the name change as well as enrollment statistics and financial data. This serves as a snapshot in time as the institution was beginning to grow into the university it is today.

The Mascot-Jefferson City zinc district of East Tennessee is the major source of zinc in the United States. Sphalerite mineralization which occurs as a breccia infilling in the Lower Ordovician Knox Group carbonates has been studied in detail at the Young Mine, located in the central portion of the district. The sphalerite occurs as fracture fillings and as rosettes between carbonate breccia blocks and displays well developed growth zoning characterized by variations in color, opacity, inclusions, and composition. Ore emplacement was preceded by two periods of solution brecciation. The first episode was related to a paleokarst terrain developed atop the Knox unconf orrni ty. The second episode was probably related to tectonic activity and expulsion of fluids from a sedimentary basin to the southeast. Episodic dolomitization in the vicinity of the ore bodies both predated and accompanied sphalerite deposition. Dolomite and other minor gangue phases deposited concurrently with sphalerite. Fluorite, calcite and quartz grew as postore, vug-filling phases. Sphalerite fluid inclusions reveal wide ranges in homogenization and freezing temperatures ( 81° to 199° C; -11.2° to -37.0° C) which may represent the mixing of two fluids--a hypersaline metal-rich brine with a less saline fluid resident in the host rocks. A geochemical model shows that Mg/Ca ratios and temperatures were such that dolomite was stable during ore deposition. Inclusions in post-ore gangue phases display an overall decrease in homogenization temperatures, are less saline, and show a narrower range of salinities. / M.S.

Diss.--Giessen (Allemagne)--Univ., 2000. / Bibliogr. p. 231-254.

Thesis (M. Sc. in Landscape design)--University of Michigan, 1935. / Typewritten. Extra numbered leaves inserted. "Shutting's Official map of Chattanooga, Tenn., c1931." "Zoning ordinance, Chattanooga, Tenn., as corrected ... by City planning commission May 21, 1926" in pocket.

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No description available.