Gabbroic Accretion
Gabbroic Accretion is a geological process in which new oceanic crust is formed at mid-ocean ridges through the sequential crystallization and emplacement of gabbroic rocks from differentiated magma chambers beneath the seafloor.
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13.8K
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711
Authors
320
Institutions
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2017–2026
31
Parents
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James B. Paces, James D. Miller · Journal of Geophysical Research Atmospheres · 1993 · 1.6K citations
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Woods Hole Oceanographic Institution
Falmouth, United States
15 h-index
31 publications
3K citations

Chinese Academy of Sciences
Beijing, China
12 h-index
48 publications
2.5K citations

Centre National de la Recherche Scientifique
Paris, France
11 h-index
26 publications
1.5K citations

Université de Montpellier
Montpellier, France
9 h-index
16 publications
928 citations
Institute of Geology and Geophysics
Beijing, China
9 h-index
32 publications
1.1K citations
University of Wyoming
Laramie, United States
9 h-index
21 publications
1.9K citations
Japan Agency for Marine-Earth Science and Technology
Yokosuka, Japan
9 h-index
11 publications
689 citations
University of Pavia
Pavia, Italy
9 h-index
14 publications
547 citations
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17 publications · 697 citations
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12 publications · 751 citations
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