Crustal Accretion
Crustal Accretion is a geophysical process in which new oceanic crust is formed through the localized intrusion and extrusion of magma at mid-ocean ridges, distinguishing it from other crustal formation mechanisms by its continuous, seafloor-spreading-driven addition of igneous material to the lithosphere.
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1.9K
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593
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Publications per year
2017–2026
114
600
Age, spreading rates, and spreading asymmetry of the world's ocean crust
R. Dietmar Müller, M. Sdrolias, Carmen Gaina et al. · Geochemistry Geophysics Geosystems · 2008 · 2.1K citations · Full text
Tectonic Implications of U-Pb Zircon Ages of the Himalayan Orogenic Belt in Nepal
Peter G. DeCelles, George E. Gehrels, Jay Quade et al. · Science · 2000 · 597 citations
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593

Chinese Academy of Sciences
Beijing, China
30 h-index
150 publications
9.6K citations
Woods Hole Oceanographic Institution
Falmouth, United States
24 h-index
60 publications
6.1K citations

Centre National de la Recherche Scientifique
Paris, France
22 h-index
74 publications
5.6K citations
Institute of Geology and Geophysics
Beijing, China
22 h-index
91 publications
5.6K citations

Chinese Academy of Geological Sciences
Beijing, China
21 h-index
53 publications
5.8K citations
United States Geological Survey
Reston, United States
19 h-index
38 publications
2.6K citations

Lamont-Doherty Earth Observatory
Sparkill, United States
18 h-index
37 publications
3.1K citations
Columbia University
New York, United States
16 h-index
29 publications
1.8K citations
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JGR · 49 publications · 4.3K citations
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46 publications · 4.8K citations
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40 publications · 3.4K citations
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30 publications · 2.8K citations
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24 publications · 3.5K citations
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