Rim Uplift

Rim Uplift is a geological structure formed by the transient displacement and permanent deformation of target materials during the excavation stage of impact cratering, distinguished by the outward and upward ejection of crustal rocks surrounding the transient cavity.

16

Publications

780

Citations

39

Authors

32

Institutions

Publications per year

2017–2026

2

Authors

39

  1. TK
    T. Kenkmann

    University of Freiburg, Germany

    3 publications · 102 citations

    3

    h-index

  2. SP
    S. P. S. Gulick

    The University of Texas at Austin, United States

    2 publications · 157 citations

    2

    h-index

  3. RA
    R. A. F. Grieve

    Geological Survey of Canada, Canada

    2 publications · 274 citations

    2

    h-index

  4. DA
    D. A. Kring

    Lunar and Planetary Institute, United States

    2 publications · 142 citations

    2

    h-index

  5. SH
    Stefan Hergarten

    University of Freiburg, Germany

    2 publications · 37 citations

    2

    h-index

1–5 of 39

Venues

  1. Meteoritics and Planetary Science

    2 publications · 153 citations

    2

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 2 publications · 142 citations

    2

    h-index

  3. Journal of Geophysical Research Planets

    2 publications · 141 citations

    2

    h-index

  4. Tectonophysics

    1 publications · 52 citations

    1

    h-index

  5. Earth and Planetary Science Letters

    1 publications · 13 citations

    1

    h-index

1–5