Forearc Basin Evolution
Forearc Basin Evolution is a geological framework that characterizes the spatiotemporal development of sedimentary basins situated between the accretionary wedge and the volcanic arc in subduction zones, distinguished by its integration of tectonic, sedimentary, and isostatic processes governing basin formation, subsidence, and stratigraphic architecture over geologic time.
637
Publications
40.9K
Citations
1.8K
Authors
665
Institutions
Publications per year
2017–2026
135
637
Serpentinization of the forearc mantle
R. D. Hyndman, Simon M. Peacock · Earth and Planetary Science Letters · 2003 · 906 citations
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University of California, Los Angeles, United States
7 publications · 670 citations
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Centre National de la Recherche Scientifique
Paris, France
26 h-index
120 publications
4.8K citations
The University of Texas at Austin
Austin, United States
18 h-index
44 publications
2.2K citations

Chinese Academy of Sciences
Beijing, China
17 h-index
48 publications
3.8K citations
University of Arizona
Tucson, United States
16 h-index
30 publications
4.2K citations
Stanford University
Stanford, United States
15 h-index
28 publications
3.5K citations

China University of Geosciences (Beijing)
Beijing, China
15 h-index
59 publications
3.4K citations
United States Geological Survey
Reston, United States
14 h-index
34 publications
2.5K citations
Institut de Recherche pour le Développement
Marseille, France
14 h-index
38 publications
1.3K citations
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60 publications · 4.8K citations
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38 publications · 2.9K citations
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37 publications · 1.9K citations
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28 publications · 2.6K citations
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20 publications · 2K citations
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