Accretionary Prism Evolution
Accretionary Prism Evolution is a geological process model that characterizes the progressive structural and stratigraphic development of a wedge-shaped accretionary complex formed at convergent plate boundaries through the accumulation, deformation, and underplating of sediments and oceanic materials scraped from a subducting tectonic plate.
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12.2K
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469
Authors
238
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2017–2026
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J. Casey Moore, P.J. Vrolijk · Reviews of Geophysics · 1992 · 496 citations
Marcus G. Langseth, J. Casey Moore · Eos · 1990 · 468 citations
Three-Dimensional Splay Fault Geometry and Implications for Tsunami Generation
Gregory F. Moore, Nathan L. Bangs, Asahiko Taira et al. · Science · 2007 · 452 citations
Timothy Kusky, Ali Polat, Brian F. Windley et al. · Earth-Science Reviews · 2016 · 423 citations · Full text
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The University of Tokyo
Tokyo, Japan
11 h-index
30 publications
2K citations
Japan Agency for Marine-Earth Science and Technology
Yokosuka, Japan
10 h-index
18 publications
3.4K citations
United States Geological Survey
Reston, United States
7 h-index
9 publications
757 citations
The University of Texas at Austin
Austin, United States
7 h-index
19 publications
4.1K citations

Lamont-Doherty Earth Observatory
Sparkill, United States
6 h-index
8 publications
1.1K citations

Cornell University
Ithaca, United States
6 h-index
11 publications
744 citations

University of Hawaii System
Honolulu, United States
6 h-index
13 publications
3.4K citations
University of Tsukuba
Tsukuba, Japan
6 h-index
6 publications
280 citations
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JGR · 9 publications · 729 citations
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8 publications · 611 citations
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