Terrane Accretion

Terrane Accretion is the tectonic process whereby a distinct fragment of crustal material, originating from a different geological setting, is added to a continental margin through plate convergence and subsequent deformation, distinguishing it from in-situ crustal growth.

1K

Publications

70.2K

Citations

2.5K

Authors

727

Institutions

Publications per year

2017–2026

163

Authors

2.5K

  1. JB
    J. Brendan Murphy

    St. Francis Xavier University, Canada

    20 publications · 1.4K citations

    18

    h-index

  2. JD
    J. Duncan Keppie

    Universidad Nacional Autónoma de México, Mexico

    18 publications · 1.3K citations

    14

    h-index

  3. CR
    C. R. L. Friend

    Australian National University, Australia

    12 publications · 1K citations

    12

    h-index

  4. GE
    George E. Gehrels

    University of Arizona, United States

    13 publications · 1.2K citations

    12

    h-index

  5. RD
    R. Damian Nance

    Ohio University, United States

    12 publications · 1K citations

    12

    h-index

1–5 of 2.5K

Venues

  1. Tectonics

    76 publications · 7.8K citations

    46

    h-index

  2. Geological Society London Special Publications

    52 publications · 6.6K citations

    40

    h-index

  3. Precambrian Research

    60 publications · 5.1K citations

    37

    h-index

  4. Geology

    51 publications · 3.8K citations

    34

    h-index

  5. Journal of the Geological Society

    JGS · 43 publications · 2.9K citations

    32

    h-index

1–5