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One more time, from the top

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  • Erik Hauri

    (Carnegie Institution of Washington)

Abstract

The formation of crust at mid-ocean ridges is generally thought to involve the ascent and melting of mantle rocks, which erupt as basalt magmas and create crust. But evidence from an ophiolite — a ridge fragment preserved on land — points to the existence of a different process. It involves incursion of sea water into the top of the mantle, and repetitive melting of rocks to create andesite magma.

Suggested Citation

  • Erik Hauri, 1999. "One more time, from the top," Nature, Nature, vol. 402(6761), pages 469-471, December.
    • Handle: RePEc:nat:nature:v:402:y:1999:i:6761:d:10.1038_44970
    DOI: 10.1038/44970
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