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Scientific literature and information products produced by Woods Hole Coastal and Marine Science Center staff

Filter Total Items: 1683

Phosphorite potential in the continental shelf off Georgia: Results of the TACTS core studies

No abstract available.
Authors
Paul Huddlestun, Vernon J. Henry, Judith A. Commeau, Jana Da Silva, F. T. Manheim, Peter Popenoe, James R. Herring

Chemical composition of ferromanganese crusts in the world ocean: a review and comprehensive database

A comprehensive database of chemical and mineralogical properties for ferromanganese crusts collected throughout the Atlantic, Pacific, and Indian Oceans, and has been assembled from published and unpublished sources which provide collection and analytical information for these samples. These crusts, their chemical compositions and natural distribution, have been a topic of interest to scientific
Authors
Frank T. Manheim, Candice M. Lane-Bostwick

Seismic-reflection data from R/V FARNELLA cruises FRNL82-7, FRNL85-1, FRNL85-2, and FRNL85-3A in the U.S. Gulf of Mexico EEZ

During the winter of 1982 and the summer and early fall of 1985, the U.S. Geological Survey (USGS) in cooperation with the Institute of Oceanographic Sciences of the United Kingdom collected approximately 30,508 line kilometers of seismic-reflection data in the U.S. Gulf of Mexico Exclusive Economic Zone (EEZ) as part of a USGS program to map the EEZ. In water depths exceeding 3,000 m, survey line
Authors
D. C. Twichell, B. A. McGregor, D.J. Lubinski

Flow separation of currents in shallow water

Flow separation of currents in shallow coastal areas is investigated using a boundary layer model for two-dimensional (depth-averaged) tidal flow past an elliptic headland. If the shoaling region near the coast is narrow compared to the scale of the headland, bottom friction causes the flow to separate just downstream of the point where the pressure gradient switches from favoring to adverse. As l
Authors
Richard P. Signell

The Blake Plateau Basin and Carolina Trough

Presently, the continental margin of the southeastern United States (Fig. 1) forms a zone of transition between the actively building, steep-fronted carbonate platform of the Bahamas and the typical eastern North American terrigenous clastic-dominated, drowned, shelf-slope-rise configuration. This region of the continental margin is underlain by two major sedimentary basins—the Blake Plateau Basin
Authors
William P. Dillon, Peter Popenoe

Mineral resources of the U.S. Atlantic continental margin

Most geologic materials may be usable resources in some form and at some time, whether it be for general land fill and aggregate, beach replenishment, construction material, or as a source of metals and fuels. Thus, most natural materials occurring within the Atlantic continental margin are resources, defined as “materials, including those only surmised to exist, that have present or anticipated f
Authors
Stanley R. Riggs, Frank T. Manheim

Options for radioactive and other hazardous waste siting within the U. S. Exclusive Economic Zone

Some areas of the E.E.Z. (Exclusive Economic Zone) offer technical, political and economic options that may complement existing approaches to hazardous waste storage and disposal.
Authors
Frank T. Manheim, Allyn Vine

Elephant teeth from the western Gulf of Maine and their implications

No abstract available.
Authors
R. N. Oldale, F.C. Whitmore, J.R. Grimes

Site 612

No abstract available. 
Authors
Claude (Wylie) Poag, Anthony B. Watts

Site 613

No abstract available.
Authors
Claude (Wylie) Poag, Anthony B. Watts

Middle to late Miocene canyon cutting on the New Jersey continental slope: Biostratigraphic and seismic stratigraphic evidence (DSDP/Site 612)

We have identified and dated a major Miocene erosional surface (M1) on the New Jersey continental slope. This surface was penetrated at Deep Sea Drilling Project (DSDP) Site 612, which was drilled near the thalweg of a buried V-shaped canyon. Biostratigraphic data at Site 612 firmly constrain the age of strata above the buried canyon surface as Zones CN7 (=NN9) and N16 (lowermost upper Miocene); t
Authors
K.G. Miller, A.J. Melillo, Gregory S. Mountain, J.A. Farre, Claude (Wylie) Poag