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.

165

Publications

12.2K

Citations

469

Authors

238

Institutions

Publications per year

2017–2026

16

Authors

469

  1. AT
    Asahiko Taira

    The University of Tokyo, Japan

    9 publications · 1.4K citations

    9

    h-index

  2. GK
    Gaku Kimura

    The University of Tokyo, Japan

    7 publications · 460 citations

    7

    h-index

  3. TB
    Tim Byrne

    University of Connecticut, United States

    6 publications · 396 citations

    6

    h-index

  4. GF
    Gregory F. Moore

    University of Hawaii System, United States

    6 publications · 1.1K citations

    6

    h-index

  5. JC
    J. Casey Moore

    University of California, Santa Cruz, United States

    6 publications · 1.3K citations

    6

    h-index

1–5 of 469

Venues

  1. Geology

    14 publications · 1.2K citations

    14

    h-index

  2. Tectonics

    13 publications · 1K citations

    13

    h-index

  3. Journal of Geophysical Research Atmospheres

    JGR · 9 publications · 729 citations

    9

    h-index

  4. Earth and Planetary Science Letters

    8 publications · 611 citations

    8

    h-index

  5. Tectonophysics

    7 publications · 652 citations

    7

    h-index

1–5