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Spreading rate dependence of gravity anomalies along oceanic transform faults

Author

Listed:
  • Patricia M. Gregg

    (Massachusetts Institute of Technology/Woods Hole Oceanographic Institution Joint Program)

  • Jian Lin

    (Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA)

  • Mark D. Behn

    (Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA)

  • Laurent G. J. Montési

    (Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA)

Abstract

Gravity and bathymetry data from transform fault systems associated with mid-ocean ridges that are spreading at different rates indicates that crustal thickening may occur under transform faults associated with intermediate- and fast-spreading ridges. If confirmed, this observation would require a change in our understanding of how magma accretion occurs along rapidly spreading mid-ocean ridges.

Suggested Citation

  • Patricia M. Gregg & Jian Lin & Mark D. Behn & Laurent G. J. Montési, 2007. "Spreading rate dependence of gravity anomalies along oceanic transform faults," Nature, Nature, vol. 448(7150), pages 183-187, July.
    • Handle: RePEc:nat:nature:v:448:y:2007:i:7150:d:10.1038_nature05962
    DOI: 10.1038/nature05962
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    Cited by:

    1. Yin, Haofei & Zhang, Aobo & Zeng, An, 2023. "Identifying hidden target nodes for spreading in complex networks," Chaos, Solitons & Fractals, Elsevier, vol. 168(C).
    2. Xiaochuan Tian & Mark D. Behn & Garrett Ito & Jana C. Schierjott & Boris J. P. Kaus & Anton A. Popov, 2024. "Magmatism controls global oceanic transform fault topography," Nature Communications, Nature, vol. 15(1), pages 1-9, December.

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