Publications
Scientific literature and information products produced by Woods Hole Coastal and Marine Science Center staff.
Filter Total Items: 1749
Mineral intergrowths replaced by "elbow-twinned" rutile in altered rocks Mineral intergrowths replaced by "elbow-twinned" rutile in altered rocks
Some aggregates of rutile, classically considered to be "elbow" twinned, instead are topotactic replacements of ilmenite or other hexagonal titaniferous precursors. Twinned rutile can be differentiated from the reticulated rutile of topotactic replacements by the angle of prism intersections, junction morphology, and the overall form of the aggregate. In a special case of topotactic...
Authors
E. R. Force, R. P. Richards, K. M. Scott, P. C. Valentine, N.S. Fishman
Seismic velocities for hydrate-bearing sediments using weighted equation Seismic velocities for hydrate-bearing sediments using weighted equation
A weighted equation based on the three-phase time-average and Wood equations is applied to derive a relationship between the compressional wave (P wave) velocity and the amount of hydrates filling the pore space. The proposed theory predicts accurate P wave velocities of marine sediments in the porosity range of 40-80% and provides a practical means of estimating the amount of in situ...
Authors
Myung W. Lee, D. R. Hutchinson, T. S. Collett, William P. Dillon
Linear alkylbenzenes as tracers of sewage-sludge-derived inputs of organic matter, PCBs, and PAHs to sediments at the 106-mile deep water disposal site Linear alkylbenzenes as tracers of sewage-sludge-derived inputs of organic matter, PCBs, and PAHs to sediments at the 106-mile deep water disposal site
Linear alkylbenzenes (LABs) are sensitive source-specific tracers of sewage inputs to the marine environment. Because they are highly particle reactive and nonspecifically sorbed to organic matter, LABs are potential tracers of the transport of both sludge-derived organic matter and other low solubility hydrophobic contaminants (e.g., PCBs and PAHs); sediment trap studies at the 106-Mile...
Authors
E.M. Lamoureux, Bruce J. Brownawell, Michael H. Bothner
Seismic reflection profile of the Blake Ridge near sites 994, 995, and 997 Seismic reflection profile of the Blake Ridge near sites 994, 995, and 997
Seismic reflection profiles near Sites 994, 995, and 997 were collected with seismic sources that provide maximum resolution with adequate power to image the zone of gas hydrate stability and the region direction beneath it. The overall structure of the sediment drift deposit that constitutes the Blake Ridge consists of southwestward-dipping strata. These strata are approximately...
Authors
William P. Dillon, Deborah R. Hutchinson, Rebecca M. Drury
Impact origin of the Chesapeake Bay structure and the source of the North American tektites Impact origin of the Chesapeake Bay structure and the source of the North American tektites
Seismic profiles, drill core samples, and gravity data suggest that a complex impact crater ~35.5 million years old and 90 kilometers in diameter is buried beneath the lower Chesapeake Bay. The breccia that fills the structure contains evidence of shock metamorphism, including impact melt breccias and multiple sets of planar deformation features (shock lamellae) in quartz and feldspar...
Authors
C. Koeberl, C. W. Poag, W.U. Reimold, D. Brandt
Character, paleoenvironment, rate of accumulation, and evidence for seismic triggering of Holocene turbidites, Canada Abyssal Plain, Arctic Ocean Character, paleoenvironment, rate of accumulation, and evidence for seismic triggering of Holocene turbidites, Canada Abyssal Plain, Arctic Ocean
Four box cores and one piston core show that Holocene sedimentation on the southern Canada Abyssal Plain for the last 8010 ± 120 yr has consisted of a continuing rain of pelagic organic and ice-rafted clastic sediment with a net accumulation rate during the late Holocene of ⩽10 mm/1000 yr, and episodically emplaced turbidites 1–5 m thick deposited at intervals of 830 to 3450 yr (average...
Authors
A. Grantz, R. L. Phillips, M. W. Mullen, S. W. Starratt, Glenn A. Jones, A.S. Naidu, B. P. Finney
Images of crust beneath southern California will aid study of earthquakes and their effects Images of crust beneath southern California will aid study of earthquakes and their effects
The Whittier Narrows earthquake of 1987 and the Northridge earthquake of 1991 highlighted the earthquake hazards associated with buried faults in the Los Angeles region. A more thorough knowledge of the subsurface structure of southern California is needed to reveal these and other buried faults and to aid us in understanding how the earthquake-producing machinery works in this region.
Authors
G. S. Fuis, D. A. Okaya, R.W. Clayton, W. J. Lutter, T. Ryberg, T.M. Brocher, T.M. Henyey, M.L. Benthien, P.M. Davis, J. Mori, R. D. Catchings, Uri S. ten Brink, M.D. Kohler, Kim D. Klitgord, R. G. Bohannon
Structural outer rim of Chesapeake Bay impact crater: Seismic and bore hole evidence Structural outer rim of Chesapeake Bay impact crater: Seismic and bore hole evidence
Nine seismic-reflection profiles and four continuous core holes define the gross structural and stratigraphic framework of the outer rim of the Chesapeake Bay impact crater. The rim is manifested as a 90 km diameter ring of terraced normal-fault blocks, which forms a ∼320 m–1200 m high rim escarpment. The top of the rim escarpment is covered by a 20 m–30 m thick ejecta blanket. The...
Authors
C. W. Poag
A precise vertical network: Establishing new orthometric heights with static surveys in Florida tidal marshes A precise vertical network: Establishing new orthometric heights with static surveys in Florida tidal marshes
Elevation differences on the order of 10 cm within Florida's marsh system influence major variations in tidal flooding and in the associated plant communities. This low elevation gradient combined with sea level fluctuation of 5-to-10 cm over decadel and longer periods can generate significant alteration and erosion of marsh habitats along the Gulf Coast. Knowledge of precise and...
Authors
E. A. Raabe, R. P. Stumpf, N.J. Marth, R.L. Shrestha
Three-dimensional models of deformation near strike-slip faults Three-dimensional models of deformation near strike-slip faults
We use three-dimensional elastic models to help guide the kinematic interpretation of crustal deformation associated with strike-slip faults. Deformation of the brittle upper crust in the vicinity of strike-slip fault systems is modeled with the assumption that upper crustal deformation is driven by the relative plate motion in the upper mantle. The driving motion is represented by...
Authors
Uri S. ten Brink, Rafael Katzman, J. Lin
Sediment distribution on a storm-dominated insular shelf, Luquillo, Puerto Rico, U.S.A. Sediment distribution on a storm-dominated insular shelf, Luquillo, Puerto Rico, U.S.A.
A sea-floor mapping investigation designed to assess the sediment distribution, the movement of the nearshore sand supply, and the fate of sediment eroded from the shoreline was conducted using high-resolution sidescan-sonar, seismic reflection, and sediment sampling techniques on the northern insular shelf of Puerto Rico, off the town of Luquillo. Sea-floor structures and the...
Authors
W. C. Schwab, R. W. Rodriguez, W.W. Danforth, M. H. Gowen