@mastersthesis {38636,
	title = {Geochemical Evolution of the Roseburg Formation Basaltic Rocks, Southern Oregon Coast Range},
	year = {1988},
	note = {Discusses the Roseburg Formation basalts, their relationship to other basalt flows in Oregon, their chemical composition and likely geologic origin (oceanic ridge / hotspot). Charts, tables, geologic maps. {\textquotedblleft}The basalt flows in the Roseburg region are mostly thick and massive with pillowed margins. Lateral gradation into pillows and pillow breccias is common. Pillows are usually 0.5 to 1.0 m in diameter and, in some areas along the North Umpqua River, they make up entire flows up to 10 m thick.{\textquotedblright} (p.28) The major professor was E. Julius Dasch.},
	pages = {142 p.},
	school = {Oregon State University},
	type = {Masters Thesis},
	edition = {M.S.},
	chapter = {Dept. of Geology},
	address = {Corvallis, Or.},
	keywords = {chemistry, Drain Or., geology, Horseshoe Bend, Jack Creek, North Umpqua River, paleosciences, Roseburg Or., theses},
	url = {https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/st74cs86z},
	author = {Pyle, Douglas G.}
}
