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Sound Waves Newsletter
Sound Waves Newsletter
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Filter Total Items: 1757
MRNIDX - Marine Data Index: Database Description, Operation, Retrieval, and Display MRNIDX - Marine Data Index: Database Description, Operation, Retrieval, and Display
A database referencing the location and content of data stored on magnetic medium was designed to assist in the indexing of time-series and spatially dependent marine geophysical data collected or processed by the U. S. Geological Survey. The database was designed and created for input to the Geologic Retrieval and Synopsis Program (GRASP) to allow selective retrievals of information...
Authors
Valerie F. Paskevich
Authigenic barite in varved clays: result of marine transgression over freshwater deposits and associated changes in interstitial water chemistry Authigenic barite in varved clays: result of marine transgression over freshwater deposits and associated changes in interstitial water chemistry
No abstract available.
Authors
Erwin Suess
A new instrument for sampling flocculent material at the water/sediment interface A new instrument for sampling flocculent material at the water/sediment interface
We have designed an instrument to collect fine-grained and flocculent material from the water/sediment interface for chemical and mineralogical analysis. The sampler can be used from a manned research submersible or by a diver in shallow water. In areas of active deposition, the material collected represents the most recently deposited sediment. This material is of interest for...
Authors
Michael H. Bothner, Page C. Valentine
The influence of a diffusive sublayer on accretion, dissolution, and diagenesis at the sea floor The influence of a diffusive sublayer on accretion, dissolution, and diagenesis at the sea floor
No abstract available.
Authors
B.P. Boudreau, N.L. Guinasso
Holocene sedimentation in the shallow nearshore zone off Nauset Inlet, Cape Cod, Massachusetts Holocene sedimentation in the shallow nearshore zone off Nauset Inlet, Cape Cod, Massachusetts
Present conditions and sedimentary evolution of the shallow offshore region near Nauset Inlet on Cape Cod, Massachusetts were clarified using high-resolution seismic-reflection profiles, sidescan-sonar records, surface grab samples and current meter measurements. The study area contains three provinces: (1) a nearshore province (shallower than 18 m) with a relatively steep slope (0.6°)...
Authors
D.G. Aubrey, D.C. Twichell, S.L. Pfirman
The nature of hydrothermal exchange between oceanic crust and seawater at 26 degrees N latitude, Mid-Atlantic Ridge The nature of hydrothermal exchange between oceanic crust and seawater at 26 degrees N latitude, Mid-Atlantic Ridge
No abstract available.
Authors
R. B. Scott, D.G. Temple, P.R. Peron
Sedimentation of lithogenic particles in the deep ocean Sedimentation of lithogenic particles in the deep ocean
Investigation of lithogenic particles collected by sediment traps in open-ocean stations revealed that the sediment flux increased linearly with depth in the water column. This rate of increase decreased with distance of the station from the continent; it was largest at the Panama Basin station and almost negligible at the E. Hawaii Abyssal Plain station. At the Panama Basin station...
Authors
S. Honjo, S.J. Manganini, L. J. Poppe
Atlantic continental margin of the United States Atlantic continental margin of the United States
The objective of this Decade of North American Geology (D-NAG) volume will be to focus on the Mesozoic and Cenozoic evolution of the U.S. Atlantic continental margin, including the onshore coastal plain, related onshore Triassic-Jurassic rift grabens, and the offshore basins and platforms. Following multiple compressional tectonic episodes between Africa and North America during the...
Authors
John A. Grow, Robert E. Sheridan
The memory of the accreting plate boundary and the continuity of fracture zones The memory of the accreting plate boundary and the continuity of fracture zones
A detailed aeromagnetic anomaly map of the Mesozoic seafloor-spreading lineations southwest of Bermuda reveals the dominant magnetic grain of the oceanic crust and the character of the accreting boundary at the time of crustal formation. The magnetic anomaly pattern is that of a series of elongate lobes perpendicular to the fracture zone (flowline) trends. The linear sets of magnetic...
Authors
Hans Schouten, Kim D. Klitgord
Oscillation of continental shelf sediments caused by waves Oscillation of continental shelf sediments caused by waves
No abstract available.
Authors
J. N. Suhayda, J. M. Coleman, Thomas Whelan, L. E. Garrison
Numerical models of hydrothermal circulation for the intrusion zone at an ocean ridge axis Numerical models of hydrothermal circulation for the intrusion zone at an ocean ridge axis
No abstract available.
Authors
P.L. Patterson, R.P. Lowell