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    Tomographic image of the magma chamber at 12°50' N on the East Pacific Rise

    THE East Pacific Rise at 12°50' N (Fig. 1) is a fast-spreading ridge with intense hydrothermal activity1, and ophiolite studies2and thermal modelling3 indicate that this is a likely setting for a magma chamber. A...

    M. S. Burnett, D. W. Caress, J. A. Orcutt in Nature (1989)