Canyon-filling debrite indicates that canyon erosion and large-scale mass movement off Georges Bank, USA, are unrelated processes

Author:

O’Leary D. W.

Publisher

Springer Netherlands

Reference6 articles.

1. EEZ-Scan 87 Scientific Staff. 1991. Atlas of the U.S. Exclusive Economic Zone, Atlantic continental margin. US Geological Survey Miscellaneous Investigations Series I-2054, 174 pp. scale 1: 500,000.

2. Emery, K.O. and Uchupi, E. 1984. The Geology of the Atlantic Ocean. Springer-Verlag, New York.

3. Farre, J.A., McGregor, B.A., Ryan, W.B.F. and Robb, J.M. 1983. Breaching the shelf-break: passage from youthful to mature phase in submarine canyon evolution. In: Stanley, D.J. and Moore, G.T. (eds) The Shelf Break: Critical Interface on Continental Margins. Society of Economic Paleontologists and Mineralogists Special Publication, 33, 25–39.

4. Lajoie, J. and St-Onge, D.A. 1985. Characteristics of two Pleistocene channel-fill deposits and their implication on the interpretation and megasequences in ancient sediments. Sedimentology, 32, 59–67.

5. O’Leary, D.W. and Dobson, M.R. 1992. Southeastern New England Continental Rise: Origin and history of slide complexes. In: Poag, C.W. and de Graciansky, P.C. (eds) Geologic Evolution of Atlantic Continental Rises. Van Nostrand Reinhold, New York, pp. 214–265.

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