Geodynamics refers to the processes by which mantle convection shapes and reshapes the Earth and other rocky planets. Its study includes plate tectonics, volcanism, the chemistry of lava and volcanic rocks, gravity and geomagnetic anomalies as well as seismic investigations into the structure of the mantle.

Latest Research and Reviews

News and Comment

  • News and Views |

    A chemically distinct region separates the Indian and Pacific mantle domains as revealed by isotope analyses on rare samples from the Australian–Antarctic Ridge.

    • Pamela D. Kempton
    Nature Geoscience 12, 151-152
  • Research Highlights |

    How the mass of super-Earths affects mantle convection is a key question for understanding rocky exoplanet structure and thermal dynamics. New material models based on ab initio mineral calculations characterize convection, with implications for magnetism, planetary cooling, atmospheric composition and habitability.

    • Tom Henshall
  • News and Views |

    During flat subduction, material is scraped off the base of the continental mantle lithosphere, building a migrating keel. This testable mechanism for flat subduction recreates features of the Laramide orogeny.

    • Marc-André Gutscher
    Nature Geoscience 11, 890-891
  • News and Views |

    The heat driving Yellowstone’s volcanism originates from a depth of at least 700 km, according to images of the mantle created using novel seismic methods.

    • Karin Sigloch
    Nature Geoscience 11, 385-387