Deborah R Hutchinson, PhD
Deborah Hutchinson is a Scientist Emeritus with the Woods Hole Coastal and Marine Science Center
Science and Products
Filter Total Items: 59
New York Bight fault New York Bight fault
High-resolution, single-channel and multichannel seismic-reflection profiles in the New York Bight provide 7 crossings of a 50-km-long fault that trends north-northeast for 30 km from its southern end, then bends northeast, and may continue northward beneath Long Island. Displacement, which is consistently down to the west, decreases upsection and suggests a growth fault. Dip of the...
Authors
Deborah R. Hutchinson, John A. Grow
Crustal structure beneath the southern Appalachians: Nonuniqueness of gravity modeling Crustal structure beneath the southern Appalachians: Nonuniqueness of gravity modeling
Gravity models computed for a profile across the long-wavelength paired negative-positive Bouguer anomalies of the southern Appalachian Mountains show that the large negative anomaly can be explained by a crustal root zone, whereas the steep gradient and positive anomaly east of the root may be explained equally well by three different geometries: a suture zone, a mantle upwarp, or a...
Authors
Deborah R. Hutchinson, John A. Grow, Kim D. Klitgord
High-resolution seismic-reflection profiles from Lake George, New York High-resolution seismic-reflection profiles from Lake George, New York
No abstract available.
Authors
Deborah R. Hutchinson
High-resolution seismic-reflection profiles and sediment samples from western Lake Ontario, New York High-resolution seismic-reflection profiles and sediment samples from western Lake Ontario, New York
No abstract available.
Authors
Deborah R. Hutchinson
The gravity field of the U.S. Atlantic continental margin The gravity field of the U.S. Atlantic continental margin
Approximately 39,000 km of marine gravity data collected during 1975 and 1976 have been integrated with U.S. Navy and other available data over the U.S. Atlantic continental margin between Florida and Maine to obtain a 10 mgal contour free-air gravity anomaly map. A maximum typically ranging from 0 to +70 mgal occurs along the edge of the shelf and Blake Plateau, while a minimum...
Authors
John A. Grow, C.O. Bowin, Deborah R. Hutchinson
Science and Products
Filter Total Items: 59
New York Bight fault New York Bight fault
High-resolution, single-channel and multichannel seismic-reflection profiles in the New York Bight provide 7 crossings of a 50-km-long fault that trends north-northeast for 30 km from its southern end, then bends northeast, and may continue northward beneath Long Island. Displacement, which is consistently down to the west, decreases upsection and suggests a growth fault. Dip of the...
Authors
Deborah R. Hutchinson, John A. Grow
Crustal structure beneath the southern Appalachians: Nonuniqueness of gravity modeling Crustal structure beneath the southern Appalachians: Nonuniqueness of gravity modeling
Gravity models computed for a profile across the long-wavelength paired negative-positive Bouguer anomalies of the southern Appalachian Mountains show that the large negative anomaly can be explained by a crustal root zone, whereas the steep gradient and positive anomaly east of the root may be explained equally well by three different geometries: a suture zone, a mantle upwarp, or a...
Authors
Deborah R. Hutchinson, John A. Grow, Kim D. Klitgord
High-resolution seismic-reflection profiles from Lake George, New York High-resolution seismic-reflection profiles from Lake George, New York
No abstract available.
Authors
Deborah R. Hutchinson
High-resolution seismic-reflection profiles and sediment samples from western Lake Ontario, New York High-resolution seismic-reflection profiles and sediment samples from western Lake Ontario, New York
No abstract available.
Authors
Deborah R. Hutchinson
The gravity field of the U.S. Atlantic continental margin The gravity field of the U.S. Atlantic continental margin
Approximately 39,000 km of marine gravity data collected during 1975 and 1976 have been integrated with U.S. Navy and other available data over the U.S. Atlantic continental margin between Florida and Maine to obtain a 10 mgal contour free-air gravity anomaly map. A maximum typically ranging from 0 to +70 mgal occurs along the edge of the shelf and Blake Plateau, while a minimum...
Authors
John A. Grow, C.O. Bowin, Deborah R. Hutchinson