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Mid-ocean-ridge seismicity reveals extreme types of ocean lithosphere

Author

Listed:
  • Vera Schlindwein

    (Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research)

  • Florian Schmid

    (Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research)

Abstract

The structure and accretion modes of two end-member types of oceanic lithosphere are described using a detailed seismicity survey along 390 kilometres of an ultraslow ridge axis, indicating deeper seismicity in amagmatic regions and explaining the uneven crustal production at ultraslow-spreading ridges.

Suggested Citation

  • Vera Schlindwein & Florian Schmid, 2016. "Mid-ocean-ridge seismicity reveals extreme types of ocean lithosphere," Nature, Nature, vol. 535(7611), pages 276-279, July.
    • Handle: RePEc:nat:nature:v:535:y:2016:i:7611:d:10.1038_nature18277
    DOI: 10.1038/nature18277
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    Cited by:

    1. 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.
    2. T. M. Morganti & B. M. Slaby & A. Kluijver & K. Busch & U. Hentschel & J. J. Middelburg & H. Grotheer & G. Mollenhauer & J. Dannheim & H. T. Rapp & A. Purser & A. Boetius, 2022. "Giant sponge grounds of Central Arctic seamounts are associated with extinct seep life," Nature Communications, Nature, vol. 13(1), pages 1-15, December.
    3. Jie Chen & Wayne C. Crawford & Mathilde Cannat, 2023. "Microseismicity and lithosphere thickness at a nearly-amagmatic oceanic detachment fault system," Nature Communications, Nature, vol. 14(1), pages 1-7, December.

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