| Title | Geochemical Evolution of the Roseburg Formation Basaltic Rocks, Southern Oregon Coast Range |
| Publication Type | Thesis |
| Year of Publication | 1988 |
| Authors | Pyle, Douglas G. |
| Academic Department | Dept. of Geology |
| Degree | M.S. |
| Pagination | 142 p. |
| University | Oregon State University |
| City | Corvallis, Or. |
| Type of Work | Masters Thesis |
| Call Number | OSU Libraries: Internet Resources LD4330 1989 .P94, Digital Open Access |
| Keywords | chemistry, Drain Or., geology, Horseshoe Bend, Jack Creek, North Umpqua River, paleosciences, Roseburg Or., theses |
| Notes | 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. “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.” (p.28) The major professor was E. Julius Dasch. |
| URL | https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/st74cs86z |
