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Sound Waves Newsletter
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Filter Total Items: 1740
Continental margins: Windows into Earth's history Continental margins: Windows into Earth's history
No abstract available.
Authors
Deborah R. Hutchinson
Sedimentary framework of Boston Harbor, Massachusetts Sedimentary framework of Boston Harbor, Massachusetts
No abstract available.
Authors
H.J. Knebel, R.R. Rendigs, R. N. Oldale, Michael H. Bothner
Ground water discharge and the related nutrient and trace metal fluxes into Quincy bay, Massachusetts Ground water discharge and the related nutrient and trace metal fluxes into Quincy bay, Massachusetts
Measurement of the rate and direction of ground water flow beneath Wollaston Beach, Quincy, Massachusetts by use of a heat-pulsing flowmeter shows a mean velocity in the bulk sediment of 40 cm d−1. The estimated total discharge of ground water into Quincy Bay during October 1990 was 1324–2177 m3 d−1, a relatively low ground water discharge rate. The tides have only a moderate effect on...
Authors
Lawrence J. Poppe, A.M. Moffett
Seismic experiment ross ice shelf 1990/91: Characteristics of the seismic reflection data Seismic experiment ross ice shelf 1990/91: Characteristics of the seismic reflection data
The Transantarctic Mountains, with a length of 3000-3500 km and elevations of up to 4500 m, are one of the major Cenozoic mountain ranges in the world and are by far the most striking example of rift-shoulder mountains. Over the 1990-1991 austral summer Seismic Experiment Ross Ice Shelf (SERIS) was carried out across the Transantarctic Mountain front, between latitudes 82 degrees to 83...
Geodetic airborne laser altimetry of Breidamerkurjökull and Skeidarárjökull, Iceland, and Jakobshavns Isbræ, West Greenland Geodetic airborne laser altimetry of Breidamerkurjökull and Skeidarárjökull, Iceland, and Jakobshavns Isbræ, West Greenland
Two geodetic airborne laser altimeter (ALA) systems coupled to Global Positioning System receivers acquired submeter-resolution topographic profiles of the lower parts of Breidamerkurjökull and Skeidarárjökull, Iceland, in May 1989 and September 1991 (Skeidarárjökull) and of Jakobshavns Isbræ, Greenland, in April 1992. Maximum measured crevasse depths on Breidamerkurjökull...
Authors
James B. Garvin, Richard S. Williams
Modeling transport processes in the coastal ocean Modeling transport processes in the coastal ocean
No abstract available.
Authors
A.F. Blumberg, R. P. Signell, H. L. Jenter
The relation between sidescan-sonar imagery and sediment physical properties: A comparison of two deep sea fan systems The relation between sidescan-sonar imagery and sediment physical properties: A comparison of two deep sea fan systems
No abstract available.
Authors
H. J. Lee, W. C. Schwab, R. E. Kayen, B. D. Edwards, D.C. Twichell, M.E. Field, J.V. Gardner
Deep Sea Drilling Project Site 612 bolide event: New evidence of a late Eocene impact-wave deposit and a possible impact site, U.S. east coast: Comment and reply Deep Sea Drilling Project Site 612 bolide event: New evidence of a late Eocene impact-wave deposit and a possible impact site, U.S. east coast: Comment and reply
No abstract available.
Authors
Wuchang Wei, C. Wylie Poag, Lawrence J. Poppe, David W. Folger, David S. Powars, Robert B. Mixon, Lucy E. Edwards, Scott Bruce
Evidence for gas accumulation associated with diapirism and gas hydrates at the head of the Cape Fear Slide Evidence for gas accumulation associated with diapirism and gas hydrates at the head of the Cape Fear Slide
Single-channel seismic reflection profiles show evidence for areas of significant gas accumulation at the head of the Cape Fear Slide on the continental rise oft North Carolina. Gas accumulation appears to occur beneath a gas hydrate seal in landward-dipping strata and in domed strata associated with diapirism. In addition, gas venting may have occurred near diapirs located at the head...
Authors
E.A. Schmuck, C. K. Paull
Lake Baikal - A touchstone for global change and rift studies Lake Baikal - A touchstone for global change and rift studies
No abstract available.
Authors
Deborah R. Hutchinson, Steve M. Colman
Modelling passive margin sequence stratigraphy Modelling passive margin sequence stratigraphy
We have modelled stratigraphic sequences to aid in deciphering the sedimentary response to sea-level change. Sequence geometry is found to be most sensitive to sea level, but other factors, including subsidence rate and sediment supply, can produce similar changes. Sediment loading and compaction also play a major role in generating accommodation, a factor often neglected in sequence...
Authors
M.S. Steckler, D. Reynolds, B. Coakley, B.A. Swift, R. D. Jarrard