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Plate Tectonics in the Caribbean

Abstract

Freeland and Dietz1 have presented a speculative geological history of the Caribbean using plate tectonic theory, and simultaneously Dickinson2 suggested that two types of plate convergence may be distinguished by examining sedimentary and tectonic evidence. Geological data from the Caribbean support much of the proposed geological history but differ in significant details. On the other hand, the Caribbean seems to fit rather well the Dickinson distinction between plate convergence types.

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References

  1. 1

    Freeland, G. L., and Dietz, R. S., Nature, 232, 20 (1971).

  2. 2

    Dickinson, W. R., Nature, 232, 41 (1971).

  3. 3

    Furrazola-Bermudez, G., Judoley, C. M., Mijailovskaya, M. S., Miroliubov, Y. S., Novojatsky, I. P., Nuñez-Jiminez, A., and Solsona, J. B., Geologia de Cuba, 239 (Inst. Cubano Recursos Minerales, Habana, 1964).

  4. 4

    Mattson, P. H., in Data for Orogenic Studies (Geol. Soc. London, Special Publ. 4, in the press).

  5. 5

    Ewing, M., Worzel, J. L., Beall, A. O., Berggren, W. A., Bukry, D., Burk, C. A., Fischer, A., and Pessagno, jun., E. A., Initial Reports of the Deep Sea Drilling Project, 1, 672 (US Government Printing Office, Washington DC, 1969).

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    JOIDES, Geotimes, 16, 12 (1971).

  7. 7

    Dengo, G., Trans. Gulf Coast Assoc. Geol. Soc., 311 (1969).

  8. 8

    Dengo, G., and Bohnenberger, O., in Tectonic Relations of North Central America and the Western Caribbean, 203 (AAPG Mem. 11, 1969).

  9. 9

    McBirney, A. R., and Bass, M. N., in Tectonic Relations of north Central America and the Western Caribbean, 203 (AAPG Mem. 11, 1969).

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