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Oceanic mafic granulite xenoliths from the Kerguelen archipelago

Nature volume 367, pages 360–363 (1994)Cite this article

Abstract

OCEANIC plateaus are large accumulations of volcanic and plutonic rocks on the ocean floor, whose detailed nature and origin are only poorly understood. Their immense volumes, frequent occurrence since the Cretaceous period1 and conspicuous presence in all major ocean basins point to their significance in understanding the Earth's thermal and chemical evolution. We report here the discovery of mafic granulite xenoliths from Kerguelen island, at the northern end of the Kerguelen plateau—one of the two largest oceanic plateaus. Granulites are normally found only in continental settings, where the crust is thick enough to experience the high temperatures and pressures required for granulite–facies minerals to form. We speculate that the Kerguelen xenoliths represent basaltic magmas underplated during the evolution of the plateau, and more generally that such mafic granulites are an important constituent of the lower parts of oceanic plateaus, which are inaccessible by drilling.

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Authors and Affiliations

  1. Université Jean Monnet, Laboratoire de Géologie-CNRS UA10, 23 rue du Docteur Paul Michelon, 42023, Saint-Etienne, Cédex 02, France

    M. Gregoire, J. Y. Cottin & A. Giret

  2. Université Libre de Bruxelles, Laboratoire de Pétrologie et Géodynamique chimique, CP 160/02, Avenue F.D. Roosevelt 50, 1050, Bruxelles, Belgium

    N. Mattielli & D. Weis

  3. Université Blaise Pascal, CNRS UA10, 5 rue Kessler, 63038, Clermont-Ferrand Cedex, France

    C. Nicollet

  4. Institut Géologique Albert-De-Lapporent, 13 Boulevard de I'Hautil, 95000, Cergy-Pontoise, France

    H. Leyrit

  5. Woods Hole Oceanographic Institution, Department of Geology and Geophysics, Woods Hole, Massachusetts, 02543, USA

    N. Shimizu

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  1. M. Gregoire
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  2. N. Mattielli
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  3. C. Nicollet
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  4. J. Y. Cottin
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  5. H. Leyrit
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  6. D. Weis
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  7. N. Shimizu
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  8. A. Giret
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Gregoire, M., Mattielli, N., Nicollet, C. et al. Oceanic mafic granulite xenoliths from the Kerguelen archipelago. Nature 367, 360–363 (1994). https://doi.org/10.1038/367360a0

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