Thesis (Ph.D.)--Oregon State University, 2000. / Includes bibliographical references (leaves 359-373).

Thesis (M.S.)--University of North Carolina at Wilmington, 2005. / Includes bibliographical references (leaves: [131]-134)

Honors Project--Smith College, Northampton, Mass., 2010. / Includes bibliographical references (p. 44-45).

Thesis (M.S.)--University of Missouri-Columbia, 2007. / The entire dissertation/thesis text is included in the research.pdf file; the official abstract appears in the short.pdf file (which also appears in the research.pdf); a non-technical general description, or public abstract, appears in the public.pdf file. Title from title screen of research.pdf file (viewed on November 6, 2007) Includes bibliographical references.

Thesis (Ph.D.)--University of Adelaide, Australian School of Petroleum, 2005? / "October 2004" Includes bibliographical references (leaves 280-291).

Thesis (M.S.)--Humboldt State University, 2008. / Two folded maps in pocket. Includes bibliographical references (leaves 90-95). Also available via Humboldt Digital Scholar.

Thesis (M.S.)--Ohio University, August, 2004. / Includes bibliographical references (p. 152-159).

Thesis (M.S.)--Ohio University, August, 2004. / Title from PDF t.p. Includes bibliographical references (p. 152-159)

Thesis (Ph. D.)--Oregon State University, 2006. / Includes map in pocket. Printout. Includes bibliographical references (leaves 170-185). Also available on the World Wide Web.

Diploma thesis deals with geological, petrological and geochemical studies of neovolcanic rocks of the SW part of the Most Basin in the area of Tušimice power plant open pit. There are two lava flows affected by coal mining in northern part of the mine. Petrological and geochemical studies with K-Ar dating relatively recent rocks in mostly weatherworn volcanic rocks showed, that they can be classified as Ti-rich basaltic rocks without olivine (tephrites), which belong to the main volcanic phase in the evolution of the Eger graben. It was evidenced geologicaly and with K-Ar dating, that studied rocks were seperated from underlying beda by hiatus which caused erosion of volcanic rocks as well as crystalline bedrock. Mmajor and trace elements composition of co-magmactic volcanics showed that rock were derived from two slightly different sources of upper mantle. Composition of two samples indicates the formation from low degree of partial melting strongly metasomatic asthenospheric mantle. Chemical features of volcanic rocks show that mantle source was comparamble to recent OIB basalts. Last sample arose from less metasomatized and depth distincted mantle which was affected by higher level of partial melting. Melts from which crystallized both rocks were minimaly affected by asimilation or...