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The growth of the North Atlantic Ocean by the spreading of its floor

Published online by Cambridge University Press:  27 October 2009

P. F. Friend
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Extract

Argument about whether or not continental drift has occurred has been continuous and inconclusive since drift was first advocated fifty years ago by scientists from a number of different disciplines. Recently, evidence has accumulated to establish beyond reasonable doubt that this drift has indeed occurred. In this paper I discuss some features of the drift, particularly those concerning the northern Atlantic Ocean. The investigations of geologists should now be turned from the question of whether drift has occurred, to the manner in which it has occurred.

Type
Articles
Information
Polar Record , Volume 13 , Issue 86 , May 1967 , pp. 579 - 588
Copyright
Copyright © Cambridge University Press 1967

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References

Bullard, E. C., Maxwell, A. E. and Revell, R. R. 1956. Heat flow through the deep sea floor. Advances in Geophysics, Vol 3, p 153–81.Google Scholar
Bullard, E. C., Everett, J. E. and Gilbert, Smith A. 1965. The fit of the continents around the Atlantic. Philosophical Transactions of the Royal Society, A, No 1088, p 41–51.Google Scholar
Funnell, B. M. 1964. Studies in north Atlantic geology and palaeontology. 1. Upper Cretaceous. Geological Magazine, Vol 101, p 421–34.Google Scholar
Gakkel', , Ya, Ya, Dementtskaya, R. M., Karasik, A. M., Isayev, E. N. and Ushakov, S. A. 1966. Morphology, physical fields and deep structure of the Arctic Basin (abstract). International Oceanographic Congress, Moscow, 1966.Google Scholar
Harland, W. B. 1961. An outline structural history of Spitsbergen. Geology of the Arctic, Vol 1, p 68–123.Google Scholar
Harland, W. B. 1965. Discussion on the tectonic evolution of the Arctic-north-Atlantic region. Philosophical Transactions of the Royal Society, A, No 1088, p 59–75.Google Scholar
Heezen, B. G., Tharp, M. and Gerard, R. D. 1961. Equatorial Atlantic fracture zones. Geological Society of America. Special Paper 68.Google Scholar
Heezen, B. G. and Ewing, M. 1961. The mid-oceanic ridge and its extension through the Arctic Basin. Geology of the Arctic, Vol 1, p 622–42.Google Scholar
Heirtzler, J. R., Le Pichon, X. and Baron, J. C. 1966. Magnetic anomalies over the Reykjanes ridge. Deep Sea Research, vol 13, p 427–44.Google Scholar
Hess, H. H. 1962. History of ocean basins. In Petrologic studies: a volume to honour A. F. Buddington, p. 599–620. Geological Society of America.Google Scholar
Johnson, L. C. and Eckhoff, D. B. 1966. Bathymetry of the North Greenland Sea. Deep-Sea Research, Vol 13, p 1161–74.Google Scholar
Koch, L., 1961. Precambrian and early palaeozoic structural elements and sedimentation: north and east Greenland. Geology of the Arctic, Vol 1, p 148–54.Google Scholar
Menard, H. W. 1966. Fracture zones and offsets of the East Pacific Rise. Journal of Geophysical Research, Vol 71, p 682–85.Google Scholar
Runcorn, S. K. 1965. Palaeomagnetic comparisons between Europe and North America. Philosophical Transactions of the Royal Society. A, No 1088, p 1–11.Google Scholar
Sykes, L. R. 1965. The seismicity of the Arctic. Bulletin of the Seismological Society of America, Vol 55, p 501–18.Google Scholar
Vine, F. J. and Matthews, D. H. 1963. Magnetic anomalies over oceanic ridges. Nature, Vol. 199, p 947–49.CrossRefGoogle Scholar
Vine, F. J. 1966. Spreading of the ocean floor; new evidence. Science, Vol 154, p 1405–15.Google Scholar
Wilson, J. T. 1965. Did the Atlantic close and then re-open? Nature, Vol 211, p 676–81.CrossRefGoogle Scholar