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Stability of active mantle upwelling revealed by net characteristics of plate tectonics

Author

Listed:
  • Clinton P. Conrad

    (SOEST, University of Hawaii at Mānoa)

  • Bernhard Steinberger

    (Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, 14473 Potsdam, Germany
    Centre for Earth Evolution and Dynamics (CEED), University of Oslo, 0316 Oslo, Norway)

  • Trond H. Torsvik

    (Centre for Earth Evolution and Dynamics (CEED), University of Oslo, 0316 Oslo, Norway
    Geodynamics, Geological Survey of Norway, NO-7491, Trondheim, Norway
    School of Geosciences, University of Witwatersrand, WITS 2050, Johannesburg, South Africa)

Abstract

Global-scale mantle flow patterns can be deduced from the net behaviour (convergence and divergence) of surface plate motions; persistent quadrupole divergence in central Africa and the central Pacific suggest sustained stationary upwelling beneath these locations in the mantle.

Suggested Citation

  • Clinton P. Conrad & Bernhard Steinberger & Trond H. Torsvik, 2013. "Stability of active mantle upwelling revealed by net characteristics of plate tectonics," Nature, Nature, vol. 498(7455), pages 479-482, June.
    • Handle: RePEc:nat:nature:v:498:y:2013:i:7455:d:10.1038_nature12203
    DOI: 10.1038/nature12203
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    Cited by:

    1. Zhidong Shi & Ross N. Mitchell & Yang Li & Bo Wan & Ling Chen & Peng Peng & Liang Zhao & Lijun Liu & Rixiang Zhu, 2024. "Sluggish thermochemical basal mantle structures support their long-lived stability," Nature Communications, Nature, vol. 15(1), pages 1-8, December.

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