Correction to “Evidence for asymmetric nonvolcanic rifting and slow incipient oceanic accretion from seismic reflection data on the Newfoundland margin”
Shillington, Donna J.
Holbrook, W. Steven
Van Avendonk, Harm J. A.
Tucholke, Brian E.
Hopper, John R.
Louden, Keith E.
Larsen, Hans Christian
Nunes, Gregory T.
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Author Posting. © American Geophysical Union, 2006. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research 111 (2006): B12403, doi:10.1029/2006JB004769.
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Evidence for asymmetric nonvolcanic rifting and slow incipient oceanic accretion from seismic reflection data on the Newfoundland margin Shillington, Donna J.; Holbrook, W. Steven; Van Avendonk, Harm J. A.; Tucholke, Brian E.; Hopper, John R.; Louden, Keith E.; Larsen, Hans Christian; Nunes, Gregory T. (American Geophysical Union, 2006-09-22)Prestack depth migrations of seismic reflection data collected around the Ocean Drilling Program (ODP) Leg 210 transect on the Newfoundland nonvolcanic margin delineate three domains: (1) extended continental crust, (2) ...
A deep seismic investigation of the Flemish Cap margin: implications for the origin of deep reflectivity and evidence for asymmetric break-up between Newfoundland and Iberia Hopper, John R.; Funck, Thomas; Tucholke, Brian E.; Louden, Keith E.; Holbrook, W. Steven; Larsen, Hans Christian (Blackwell Publishing, 2006-02-21)Seismic reflection and refraction data were acquired along the southeast margin of Flemish Cap at a position conjugate to drilling and geophysical surveys across the Galicia Bank margin. The data document first-order ...
Seismic reflection, magnetic, and gravity profiles of the eastern Atlantic continental margin and adjacent deep-sea floor. II. Congo Canyon (Republic of Zaire) to Lisbon (Portugal) Uchupi, Elazar; Emery, Kenneth O. (Woods Hole Oceanographic Institution, 1974-04)One of the programs of the International Decade of Ocean Exploration (I.D.O.E.) is a geological and geophysical study of the eastern Atlantic continental margin and adjacent deep-sea floor. This report is a compilation of ...