Index Catalog // ScholarsArchive@OSU

Tectonics of the East Pacific Rise, 5⁰ to 12⁰S

Creator:: Rea, David K.
Abstract:: The portion of the East Pacific Rise (EPR) between 5° and 12°S can be subdivided into three areas by fracture zones that offset the rise axis at about 6.5°S and 9°S. In all three regions, the spreading axis of the EPR is defined by a topographic block 300 to 350...
Resource Type:: Dissertation
Full Text:: Isochron 41 Regional Structure of the Ocean Floor 44 A Fossil Axial Block and Its Implications 49 Seamounts

Temperatures and compositions of magmas ascending beneath actively spreading mid-ocean ridges

Creator:: Scheidegger, Kenneth Fred
Resource Type:: Dissertation
Full Text:: ) Title: TEMPERATURES AND COIVJPOSITIONS OP MAGMAS AZCENDING BENEATH ACTIVELY SPREADI,N ID-OCEAN RIDGES

Deposition of submarine hydrothermal manganese and iron, and evidence for hydrothermal input of volatile elements to the ocean

Creator:: Toth, John R.
Abstract:: File scanned at 300 ppi (Monochrome) using ScandAll PRO 1.8.1 on a Fi-6670 in PDF format. CVista PdfCompressor 4.0 was used for pdf compression and textual OCR.
Resource Type:: Masters Thesis
Full Text:: OCEAN The chemical and mineralogical analysis of manganese-rich and iron rich oxide crusts, of

On the influence of terrestrial heat flow anomalies on the temperature microstructure at the ocean floor

Creator:: Vossler, Donald Alan
Abstract:: The effects on the temperature microstructure of terrestrial heat flow and heat flow anomalies at the ocean floor are discussed on the basis of a simple heat diffusion model. The effects on the temperature microstructure of layering of the thermal properties of the ocean are investigated. This is done both...
Resource Type:: Masters Thesis
Full Text:: diffusion of suspended particles near the ocean bottom. Deep Sea Research 13: 679-685. Isaacs, J. D., J. L

On the reduction and interpretation of ocean-floor temperature and heat flow data

Creator:: Shih, Keh-gong
Abstract:: In this thesis, the interpretation and reduction of ocean heat flow measurements are discussed on the basis of theoretical models. The instrument effect x heat flow measurements is investigated for the case of long period measurements by studying the heat conduction along the measurement probe for both steady and unsteady...
Resource Type:: Dissertation
Full Text:: 1 Measurement of Heat Flow at the Ocean Bottom 1 Physical Constants Within the Crust and Upper

Magnetic and gravity interpretation of Yaloc-69 data from the Cocos plate area

Creator:: Lu, Richard Shih-Ming
Abstract:: Magnetic, gravity and bathymetry data were collected on an extended cruise of the R/V Yaquina in 1969. The last set of data was obtained from those track lines leaving the Panama Basin. The area covered is mainly the Cocos plate (Molnar and Sykes, 1969). The data is analyzed and compared...
Resource Type:: Masters Thesis
Full Text:: from this set of data; fur- ther detailed study of more track lines and sea bottom core samples are

Some aspects of the biology of the deep sea holothuroid Paelopatides sp.

Creator:: Hufford, Gary L.
Resource Type:: Masters Thesis
Full Text:: collected seasonally. Paelopatides sp. , a bottom - dweller feeding on surface sediment, is found to spawn

Ocean Globe : Foreword

Creator:: Wright, Dawn J.
Abstract:: Keywords: ocean science, bathymetry, geographic information systems, marine science, ocean exploration
Resource Type:: Part of Book
Full Text:: vantage, the Earth is indeed an “ocean globe,” with 72 percent of its surface covered by a fluid enve

Oceanic vertical temperature measurements across the water-sediment interface at selected stations west of Oregon

Creator:: Mesecar, Roderick S.
Resource Type:: Dissertation
Full Text:: the ocean bottom interface for 19 stations west of Depoe Bay, Oregon. The station locations are

A study of turbulence in the viscous sublayer and logarithmic region of the bottom boundary layer

Creator:: Chriss, Terry Michael
Abstract:: Detailed current profiles between the sediment-water interface and 20 cm above it reveal a viscous sublayer in the bottom boundary layer on the Oregon continental shelf. Data from three field experiments are used to test fundamental assumptions about boundary layer flow in the ocean. The first study, discussed in Chapter...
Resource Type:: Dissertation
Full Text:: Viscous Sublaver and Logarithmic Region of the Bottom Boundary Layer abstract approved: D. Caidwell

ScholarsArchive@OSU

Tectonics of the East Pacific Rise, 5⁰ to 12⁰S

Temperatures and compositions of magmas ascending beneath actively spreading mid-ocean ridges

Deposition of submarine hydrothermal manganese and iron, and evidence for hydrothermal input of volatile elements to the ocean

On the influence of terrestrial heat flow anomalies on the temperature microstructure at the ocean floor

On the reduction and interpretation of ocean-floor temperature and heat flow data

Magnetic and gravity interpretation of Yaloc-69 data from the Cocos plate area

Some aspects of the biology of the deep sea holothuroid Paelopatides sp.

Ocean Globe : Foreword

Oceanic vertical temperature measurements across the water-sediment interface at selected stations west of Oregon

A study of turbulence in the viscous sublayer and logarithmic region of the bottom boundary layer

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