Back-arc Basins
Back-Arc Basin is a type of extensional oceanic basin that forms behind a volcanic arc at a convergent plate boundary, distinguished from other basins by its development through subduction-induced mantle flow and lithospheric stretching in response to trench rollback.
680
Publications
56.7K
Citations
2.2K
Authors
721
Institutions
Publications per year
2017–2026
146
Variants
Back-arc Basin
Parents
680
Back‐arc opening and the mode of subduction
Seiya Uyeda, Hiroo Kanamori · Journal of Geophysical Research Atmospheres · 1979 · 1.3K citations · Full text
Accretionary orogens through Earth history
Peter A. Cawood, Alfred Kröner, William J. Collins et al. · Geological Society London Special Publications · 2009 · 1.1K citations
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2.2K
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National Institute of Water and Atmospheric Research, New Zealand
10 publications · 883 citations
10
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9
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9
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1–5 of 2.2K
721
The University of Tokyo
Tokyo, Japan
27 h-index
85 publications
7K citations

Centre National de la Recherche Scientifique
Paris, France
25 h-index
79 publications
6.4K citations

Chinese Academy of Sciences
Beijing, China
21 h-index
86 publications
5.9K citations

Australian National University
Canberra, Australia
20 h-index
42 publications
4.3K citations

Sorbonne Université
Paris, France
18 h-index
37 publications
3.4K citations
Japan Agency for Marine-Earth Science and Technology
Yokosuka, Japan
18 h-index
47 publications
3K citations
Roma Tre University
Rome, Italy
15 h-index
29 publications
2.8K citations
Geological Survey of Japan
Tsukuba, Japan
15 h-index
26 publications
1.9K citations
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54 publications · 4.2K citations
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46 publications · 5.3K citations
33
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38 publications · 4.8K citations
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JGR · 27 publications · 6.9K citations
24
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27 publications · 2.6K citations
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