Continental Drift

Continental Drift is a geodynamic hypothesis in Earth sciences that posits that Earth’s continental lithospheric masses have undergone long-term, large-scale horizontal displacement relative to one another across the planet’s surface through geological time, thereby reorganizing paleogeographic and biogeographic patterns.

1.3K

Publications

81.4K

Citations

2.8K

Authors

893

Institutions

Publications per year

2017–2026

141

Authors

2.8K

  1. MR
    Michele Rebesco

    National Institute of Oceanography and Applied Geophysics, Italy

    15 publications · 1K citations

    14

    h-index

  2. DA
    Dorrik A. V. Stow

    Heriot-Watt University, United Kingdom

    14 publications · 1K citations

    14

    h-index

  3. FJ
    F. Javier Hernández‐Molina

    Royal Holloway University of London, United Kingdom

    14 publications · 686 citations

    13

    h-index

  4. JE
    James E T Channell

    University of Florida, United States

    11 publications · 695 citations

    11

    h-index

  5. GU
    Gabriele Uenzelmann‐Neben

    Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Germany

    11 publications · 433 citations

    11

    h-index

1–5 of 2.8K

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 46 publications · 6.4K citations

    31

    h-index

  2. Geological Society London Special Publications

    41 publications · 3K citations

    29

    h-index

  3. Marine Geology

    44 publications · 2.1K citations

    28

    h-index

  4. Nature

    49 publications · 4.7K citations

    26

    h-index

  5. Science

    33 publications · 2.9K citations

    25

    h-index

1–5