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.
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Publications
81.4K
Citations
2.8K
Authors
893
Institutions
Publications per year
2017–2026
141
1.3K
Sea-floor spreading and continental drift
Xavier Le Pichon · Journal of Geophysical Research Atmospheres · 1968 · 1.5K citations
A New Class of Faults and their Bearing on Continental Drift
J. Tuzo Wilson · Nature · 1965 · 1.3K citations
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National Institute of Oceanography and Applied Geophysics, Italy
15 publications · 1K citations
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Royal Holloway University of London, United Kingdom
14 publications · 686 citations
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11
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Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Germany
11 publications · 433 citations
11
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893

Centre National de la Recherche Scientifique
Paris, France
29 h-index
99 publications
7.4K citations

Lamont-Doherty Earth Observatory
Sparkill, United States
19 h-index
31 publications
3.9K citations
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Bremerhaven, Germany
19 h-index
44 publications
1.7K citations
National Institute of Oceanography and Applied Geophysics
Trieste, Italy
18 h-index
52 publications
3.6K citations

British Antarctic Survey
Cambridge, United Kingdom
18 h-index
33 publications
3.5K citations

Chinese Academy of Sciences
Beijing, China
18 h-index
97 publications
9.5K citations
Columbia University
New York, United States
17 h-index
28 publications
3.7K citations
Woods Hole Oceanographic Institution
Falmouth, United States
16 h-index
26 publications
2.1K citations
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JGR · 46 publications · 6.4K citations
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41 publications · 3K citations
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44 publications · 2.1K citations
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49 publications · 4.7K citations
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33 publications · 2.9K citations
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