Abstract
IT has been proposed1–3 that the opening of the Bay of Biscay occurred by rotation about a pole situated near Paris (50.0° N, 3.3° E) and not about the pole proposed by Bullard et al.4 (43.6° N, 1.0° E). The rotation about the first pole results in strike-slip motion along the North Pyrenean Fault during the pre-Upper-Cretaceous opening, while the rotation about the second pole results in compression there. The second rotation is not compatible with geological data5 which indicates extension prior to Upper Cretaceous in the Pyrenean region.
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References
Le Pichon, X., Bonnin, J., and Sibuet, J. C., CR Acad. Sci., 271, 1941 (1970).
Le Pichon, X., Bonnin, J., Francheteau, J., and Sibuet, J. C., Une hypothèse d'evolution tectonique du golfe de Gascogne. Symp. sur l'histoire structurale du golfe de Gascogne, Rueil-Malmaison (in the press).
Le Pichon, X., and Sibuet, J. C., Earth Planet. Sci. Lett. (in the press).
Bullard, E. C., Everett, J. E., and Smith, A. G., Phil. Trans. Roy. Soc., A, 258, 41 (1965).
Mattauer, M., Earth Planet. Sci. Lett., 7, 87 (1969).
Williams, C. A., and McKenzie, D., Nature, 232, 168 (1971).
Le Borgne, E., and Le Mouël, J., CR Acad. Sci., 271, 1167 (1970).
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LE PICHON, X., SIBUET, JC. Comments on the Evolution of the North-East Atlantic. Nature 233, 257–258 (1971). https://doi.org/10.1038/233257a0
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DOI: https://doi.org/10.1038/233257a0
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