Abstract
Rifts occur at all stages of the Wilson Cycle of opening and closing of oceans, but those most likely to be preserved form either at continental breakup or continental collision. All preserved rifts are “failed rifts” because they have not “succeeded” in developing into oceans. Hundreds of ancient rifts ranging up to 2.6 Ga in age have been recognized. Axial mafic dike systems have been located in both ancient and active rifts and activation of the basalt-eclogite transition in these systems may be an effective way of promoting the repeated subsidence that characterizes many rift complexes, such as those of the North Sea. Ancient rifts striking into fold belts are known as aulacogens (after Shatski). Recognition (after Wilson) that many fold belts mark places where oceans have closed has made it possible to interpret numerous aulacogens as rifts formed at continental rupture and to interpret their history in plate-tectonic terms. In many ways the best known of rift systems are those formed at the opening of the Atlantic Ocean because they have been subjected to intense petroleum exploration. Eleven classes of rifts with diverse histories can be distinguished among the rifts presently facing Atlantic-type continental margins and aulacogen histories are even more diverse.
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References
J.T. Wilson,Nature, 207, 343, 1965.
J.T. Wilson,EOS, 58, 366, 1977.
J.T. Wilson,Proc. Am. Philos. Soc., 112, 309, 1968.
J.F. Dewey and K. Burke,Geology, 2, 57, 1974.
K. Burke,Tectonophysics, 36, 96, 1976.
R. Thiessen, K. Burke and W.S.F. Kidd, EOS, 58, 503, 1977.
K. Burke,Tectonophysics, 36, 197, 1976.
K. Burke and A.J. Whiteman, Rifting and the Breakup of Africa, in: Implications of Continental Drift to the Earth Sciences, ed. by D.H. Tarling and S.K. Runcorn, Acadmic London, 1973.
K. Burke and J.F. Dewey, J. Geol., 81, 406, 1973.
K. Burke, Ann. Rev. Earth Planet. Sci., 5, 371, 1977.
A.M.C. Sengor, Geology, 4, 779, 1976.
P. Molnar and P. Tapponnier, Science, 189, 419, 1975.
K. Burke and F.J. Sawkins, in press.
J.F. Dewey and W.S.F. Kidd, Geology, 2, 543, 1974.
N. Schatski, Vergleichende Tektonik alter Tafeln, Akademie, Berlin, 1961.
J.F. Dewey and A.M.C. Sengor, in press.
J.F. Dewey, W.C. Pitman, W.B.F. Ryan and J. Bonnin, Geol. Soc. Am. Bull., 84, 3137, 1973.
A. Gansser, Geology of the Himalayas, Wiley, London, 1964.
R. Steele,Tectonophysics 36, 207, 1976.
R.B. McConnell, Geol. Rundsch., 63, 389, 1974.
A.W. Woodland, ed., Petroleum and the Continental Shelf of Northwest Europe, Wiley, London, 1975.
K. Burke, J.F. Dewey and W.S.F. Kidd,Tectonophysics, 40, 69, 1977.
K. Burke, J.F. Dewey and W.S.F. Kidd, Dominance of Horizontal Movements, Arcf and Microcontinental Collision, in: The Early History of the Earth, ed. by B.F. Windley, Wiley, London,
F.J. Sawkins, Geology, 4, 427, 1976.
J.D. Sclater, S. Hellinger and C. Tapscott, EOS, 58, 367,1977
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© 1978 D. Reidel Publishing Company, Dordrecht, Holland
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Burke, K. (1978). Evolution of Continental Rift Systems in the Light of Plate Tectonics. In: Ramberg, I.B., Neumann, ER. (eds) Tectonics and Geophysics of Continental Rifts. NATO Advanced Study Institutes Series, vol 37. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-9806-3_1
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DOI: https://doi.org/10.1007/978-94-009-9806-3_1
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