Index Catalog // ScholarsArchive@OSU

Creator:: Leinen, Margaret, 1946-
Abstract:: A new technique for determining the amount of opal in deep-sea sediments of any age is described. Using a normative calculation, a portion of the analytical silica concentration of sediments is subtracted as non-biogenic in proportion to the concentration of aluminum in the sample. The ratio of SiO₂:Al₂O₃ used to...
Resource Type:: Masters Thesis
Full Text:: AN ABSTRACT OF THE THESIS OF Margaret Leinen for the degree of

Creator:: Krissek, Lawrence A.
Abstract:: Holocene hemipelagic deposition of terrigenous silts and clays dominates sedimentation on most of the Oregon and Washington continental slope. The sources of these sediments, the mechanisms causing sediment dispersal, and the relative contributions of the various continental sources to the marine deposits have been investigated using quantitative mineral and geochemical...
Resource Type:: Dissertation
Full Text:: urn fraction of the fluvial sediments, but may form 25-50% of the <2 m fraction in some source areas

Creator:: Oregon State College. School of Oceanography
Abstract:: This compilation by the School of Oceanography of Oregon State University lists in chronological order the oceanographic reports published in 1975 and 1976. It also lists theses for which degrees were awarded in 1976. This is the third annual update of our reference 74-1 which brought together a listing of...
Resource Type:: Technical Report
Full Text:: 75-12 L. Gordon L. Barstow M. Lilley E. Seifert P.K. Park 75-13 N.C. Yao S. Neshyba H. Crew 75-14 P

Creator:: Lyle, Mitchell
Resource Type:: Dissertation
Full Text:: . Landa, E.R.,, and Gast, R.G. Clays Clay Miner. 21, 121-130 (1973). 8. Leinen, M. Geochim. Cosmochini

Creator:: Moser, John Christian
Resource Type:: Masters Thesis
Full Text:: core profiles formed by using both near-surface samples from the multiple gravity core (M) and deeper

Creator:: Stakes, Debra S.
Resource Type:: Dissertation
Full Text:: no vermiculite. Plagioclase remains quite fresh in these samples except for traces of apatite (M

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