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The structure and tectonics of the Blanco Fracture Zone

Creator:: Ibach, Darrell Henry
Resource Type:: Masters Thesis
Full Text:: northeast Pacific ocean showing the area of overriding of the Juan de Fuca plate by the Pacific plate at the

Gravity and structures of the crust and subcrust in the northeast Pacific Ocean west of Washington and British Columbia

Creator:: Couch, Richard W.
Resource Type:: Dissertation
Full Text:: km to the north. Hess (1964) attributed variations in mantle velocities in the Pacific Ocean to

Gravity and structures of the crust and subcrust in the northeast Pacific Ocean west of Washington and British Columbia

Creator:: Couch, Richard W.
Resource Type:: Dissertation
Full Text:: STRUCTURES OF THE CRUST AND SUB- CRUST IN THE NORTHEAST PACIFIC OCEAN WEST OF WASHINGTON AN Abstract

Diffuse deformation patterns along the North American plate boundary zone, offshore western United States

Creator:: Chaytor, Jason D.
Abstract:: Plate boundaries are commonly regions of complex, diffuse deformation with the motion across the boundary accommodated by numerous structural systems, rather than being narrow, discrete zones of deformation. One such boundary occurs where the North American plate makes contact with Juan de Fuca, Gorda, and Pacific plates along the west...
Resource Type:: Dissertation
Full Text:: Tectonic evolution of the Pacific-Farallon-North American plate boundary during the mid to late

Tertiary geologic framework, neotectonics, and petroleum potential of the Oregon-Washington Continental Margin

Creator:: Snavely, P. D., Jr. and Geological Survey (U.S.)
Abstract:: The Tertiary geologic evolution of the Oregon and Washington continental margin was molded by episodic periods of convergence between the Pacific oceanic plates and the North American plate. This margin is the site of a deep basin that is floored by Paleocene to lower Eocene oceanic crust and contains more...
Resource Type:: Part of Book
Full Text:: between the Pacific oce anic plates and the North American plate. This margin is the site of a deep basin

Holocene and latest Pleistocene paleoceanography of the northeast Pacific and its relationship to climate change in the Pacific Northwest

Creator:: Sabin, Ann Louise
Abstract:: Northeast Pacific Ocean sediments were analyzed to determine the past relationship between northeast Pacific sea surface conditions and the climate on the adjacent continent, the Pacific Northwest of North America. Studies of modern ocean-atmosphere interactions demonstrate the significant effect sea surface conditions and atmospheric circulation in the Northeast Pacific Ocean...
Resource Type:: Masters Thesis

Structure and tectonics of Cascadia segment, Central blanco transform fault zone

Creator:: deCharon, Annette V.
Resource Type:: Masters Thesis

Paleomagnetic inclination shallowing in deep-sea sediments

Creator:: Arason, Pórdur
Abstract:: In this thesis anomalous downcore shallowing of paleomagnetic inclinations is interpreted to be caused by sediment compaction. Thus, compaction-induced inclination shallowing may influence tectonic reconstructions that are based on inclinations from deep-sea sediment cores. Progressive downcore shallowing of the remanent inclination was observed in a 120-m section of Plio- Pleistocene...
Resource Type:: Dissertation
Full Text:: From the Pacific Ocean 2.1 Introduction 9 2.2 Data From Pacific Ocean Sediments 12 2.3 Data Analysis 21

Coastal transition zone pilot - 1987 : rapid sampling vertical profiler observations

Creator:: Park, Melora M., Moum, James N., Caldwell, Douglas R., and Oregon State University. College of Oceanography
Abstract:: Temperature, salinity, sigma-t and dissipation profiles from the Rapid Sampling Vertical Profiler for six transects as part of the Coastal Transition zone pilot experiment, June 1987.
Resource Type:: Technical Report
Full Text:: characteristics of the transition region between coastal upwelling and open ocean off the west coast of North

Temperature finestructure and microstructure observations in the coastal upwelling region off Oregon during the summer of 1974

Creator:: Marmorino, G. O.
Resource Type:: Dissertation
Full Text:: LIST OF FIGURES Figure Page 1 Location of 100 in station 5 2 Summer 1974 north-south winds as

ScholarsArchive@OSU

The structure and tectonics of the Blanco Fracture Zone

Gravity and structures of the crust and subcrust in the northeast Pacific Ocean west of Washington and British Columbia

Gravity and structures of the crust and subcrust in the northeast Pacific Ocean west of Washington and British Columbia

Diffuse deformation patterns along the North American plate boundary zone, offshore western United States

Tertiary geologic framework, neotectonics, and petroleum potential of the Oregon-Washington Continental Margin

Holocene and latest Pleistocene paleoceanography of the northeast Pacific and its relationship to climate change in the Pacific Northwest

Structure and tectonics of Cascadia segment, Central blanco transform fault zone

Paleomagnetic inclination shallowing in deep-sea sediments

Coastal transition zone pilot - 1987 : rapid sampling vertical profiler observations

Temperature finestructure and microstructure observations in the coastal upwelling region off Oregon during the summer of 1974

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