Accretionary Complexes
Accretionary Complexes is a geological structure formed at convergent plate margins that consists of fragmented and deformed sedimentary and oceanic materials scraped off a subducting tectonic plate and accreted onto the overriding plate, distinguished from other tectonic assemblages by its chaotic stratigraphy, melange fabric, and structural imbrication resulting from prolonged subduction processes.
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Oregon Subduction Zone: Venting, Fauna, and Carbonates
L. D. Kulm, Erwin Suess, J. Casey Moore et al. · Science · 1986 · 487 citations
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Chinese Academy of Sciences
Beijing, China
22 h-index
127 publications
8.5K citations
The University of Tokyo
Tokyo, Japan
22 h-index
66 publications
3.9K citations
Japan Agency for Marine-Earth Science and Technology
Yokosuka, Japan
21 h-index
63 publications
3.6K citations
Geological Survey of Japan
Tsukuba, Japan
18 h-index
36 publications
1.7K citations

Kōchi University
Kochi, Japan
18 h-index
38 publications
1.8K citations
Institute of Geology and Geophysics
Beijing, China
18 h-index
93 publications
5.7K citations
Tokyo Institute of Technology
Tokyo, Japan
18 h-index
55 publications
5.8K citations
Xinjiang Institute of Ecology and Geography
Ürümqi, China
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40 publications
1.9K citations
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JGR · 32 publications · 3.2K citations
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