Skip to main content
U.S. flag

An official website of the United States government

Publications

Filter Total Items: 7518

Leg 84 of the Deep Sea Drilling Project Leg 84 of the Deep Sea Drilling Project

No abstract available.
Authors
J. Aubouin, Roland E. von Huene, M. Baltuck, Robert Arnott, J. Bourgois, M.V. Filewicz, Keith A. Kvenvolden, Barry Leinert, Tom McDonald, Kristin McDougall-Reid, Y. Ogawa, Elliot Taylor, Barbara Winsborough

Implementation of digital subtraction angiography with a synchrotron x-ray beam Implementation of digital subtraction angiography with a synchrotron x-ray beam

The intense synchrotron radiation produced by wiggler magnets at electron storage rings provides a new source of x-rays highly suited to iodine K-edge digital subtraction angiography. The monochromaticity and tunability provide maximum sensitivity to intraarterial iodine and virtually eliminate contrast due to soft tissue and bone. Visualization of arteries, in particular the coronary...
Authors
H.D. Zeman, E.B. Hughes, L.E. Campbell, R. Hofstadter, Randolph L. Kirk, T.J. Krolicki, J. Rolfe, J.P. Stone, S. Wilson, E. Rubenstein, A.C. Thompson, J.T. Walton

Ancient plate boundaries in the Bering Sea region Ancient plate boundaries in the Bering Sea region

Plate tectonic models of the Bering Sea suggest that the abyssal Bering Sea Basin is underlain by oceanic crust, a supposition supported by refraction and magnetic data. The oceanic crust is thought to be a remnant of the Kula(?) plate that was isolated within what is now the Bering Sea when the proto-Aleutian arc began to form between the Alaska Peninsula and Kamchatka in late Mesozoic...
Authors
M. S. Marlow, Alan K. Cooper, David W. Scholl, H. McLean

Spurs and grooves revisited: construction versus erosion, Looe Key Reef, Florida Spurs and grooves revisited: construction versus erosion, Looe Key Reef, Florida

Six of 12 core holes drilled at Looe Key Reef (24°37'18"N. 81°24'24"W) by a diver-operated coring device penetrated a spur and groove system. Drilling indicated that: (II the spurs and grooves formed over at least 5 m of carbonate reef sand: (2) the underlying Pleistocene surface is essentially flat and therefore could not control or initiate spacing of spurs or grooves; (3) only the...
Authors
E.A. Shinn, J.H. Hudson, Daniel M. Robbin, Barbara H. Lidz

The geology of Europa The geology of Europa

The map units and lineations of Europa are detailed, and the geologic processes, and history, and thick and thin ice models of the satellite are discussed. It is concluded that Europa lacks evidence of a horizontally stratified crust; the geology appears characterized by disruption of the crust and intrusions into an icy shell. The surface consists of plains and mottled terrain, the...
Authors
Baerbel K. Lucchitta, Laurence A. Soderblom

Geomagnetic local and regional harmonic analyses Geomagnetic local and regional harmonic analyses

Procedures are developed for using rectangular and cylindrical harmonic analyses in local and regional areas. Both the linear least squares analysis, applicable when component data are available, and the nonlinear least squares analysis, applicable when only total field data are available, are treated. When component data are available, it is advantageous to work with residual fields...
Authors
L.R. Alldredge

Erosional channels on the shoreface of Nauset Beach, Cape Cod, Massachusetts Erosional channels on the shoreface of Nauset Beach, Cape Cod, Massachusetts

Many channels (1 to 3 m relief)_are located offshore of Nauset Beach, Cape Cod, Massachusetts, in water 4 to 18 m deep. The channels are oblique to the shoreline, are spaced approximately 260 m apart, and deepen seaward. The southern flank of each channel is rippled whereas the northern flank and interchannel areas are smooth. The origin of the channels is unknown. They probably formed...
Authors
S. W. Needell, William P. Dillon, H.J. Knebel

Morphology, distribution, and development of submarine canyons on the United States Atlantic continental slope between Hudson and Baltimore Canyons Morphology, distribution, and development of submarine canyons on the United States Atlantic continental slope between Hudson and Baltimore Canyons

The distribution and morphology of submarine canyons off the eastern United States between Hudson and Baltimore Canyons have been mapped by long-range sidescan sonar. In this area canyons are numerous, and their spacing correlates with overall slope gradient; they are absent where the gradient is less than 3°, are 2 to 10 km apart where the gradient is 3° to 5°, and are 1.5 to 4 km apart...
Authors
David C. Twichell, David G. Roberts

Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: October 1982 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: October 1982

The preliminary geomagnetic data included here is made available to scientific personnel and organizations, as part of a cooperative effort and on a data exchange basis because of the early need by some users. To avoid delay, all of the data is copied from original forms processed at the observatory; therefore it should be regarded as preliminary.
Authors
John B. Townshend, J.E. Papp, E.A. Sauter, L.Y. Torrence, T.K. Cunningham

Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: March 1982 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: March 1982

The preliminary geomagnetic data included here is made available to scientific personnel and organizations, as part of a cooperative effort and on a data exchange basis because of the early need by some users. To avoid delay, all of the data is copied from original forms processed at the observatory; therefore it should be regarded as preliminary.
Authors
John B. Townshend, J.E. Papp, E.A. Sauter, L.Y. Torrence
Was this page helpful?