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Geophysical evidence for reduced melt production on the Arctic ultraslow Gakkel mid-ocean ridge

Author

Listed:
  • W. Jokat

    (Alfred Wegener Institute for Polar and Marine Research, Columbusstrasse)

  • O. Ritzmann

    (Alfred Wegener Institute for Polar and Marine Research, Columbusstrasse)

  • M. C. Schmidt-Aursch

    (Alfred Wegener Institute for Polar and Marine Research, Columbusstrasse)

  • S. Drachev

    (VNIIOkeangeologia)

  • S. Gauger

    (Alfred Wegener Institute for Polar and Marine Research, Columbusstrasse)

  • J. Snow

    (Max-Planck-Institut für Chemie)

Abstract

Most models of melt generation beneath mid-ocean ridges1,2,3 predict significant reduction of melt production at ultraslow spreading rates (full spreading rates

Suggested Citation

  • W. Jokat & O. Ritzmann & M. C. Schmidt-Aursch & S. Drachev & S. Gauger & J. Snow, 2003. "Geophysical evidence for reduced melt production on the Arctic ultraslow Gakkel mid-ocean ridge," Nature, Nature, vol. 423(6943), pages 962-965, June.
    • Handle: RePEc:nat:nature:v:423:y:2003:i:6943:d:10.1038_nature01706
    DOI: 10.1038/nature01706
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    Cited by:

    1. Christopher R. German & Eoghan P. Reeves & Andreas Türke & Alexander Diehl & Elmar Albers & Wolfgang Bach & Autun Purser & Sofia P. Ramalho & Stefano Suman & Christian Mertens & Maren Walter & Eva Ram, 2022. "Volcanically hosted venting with indications of ultramafic influence at Aurora hydrothermal field on Gakkel Ridge," Nature Communications, Nature, vol. 13(1), pages 1-11, December.
    2. John M. O’Connor & Wilfried Jokat & Peter J. Michael & Mechita C. Schmidt-Aursch & Daniel P. Miggins & Anthony A. P. Koppers, 2021. "Thermochemical anomalies in the upper mantle control Gakkel Ridge accretion," Nature Communications, Nature, vol. 12(1), pages 1-12, December.

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