Truncation Surfaces

Truncation Surface is a stratigraphic surface formed by the erosion or non-deposition that terminates underlying sedimentary layers, distinguishing it from other stratigraphic surfaces by marking a distinct break in the depositional sequence due to subaerial exposure or marine erosion.

32

Publications

1.6K

Citations

80

Authors

46

Institutions

Publications per year

2017–2026

6

Authors

80

  1. SE
    Ståle Emil Johansen

    Norwegian University of Science and Technology, Norway

    2 publications · 40 citations

    2

    h-index

  2. KH
    Kyrre Heldal Kartveit

    Norwegian University of Science and Technology, Norway

    2 publications · 40 citations

    2

    h-index

  3. MN
    Marinos N. Vouvakis

    University of Massachusetts Amherst, United States

    2 publications · 107 citations

    2

    h-index

  4. EA
    Erick A. Bestland

    Flinders University, Australia

    2 publications · 87 citations

    2

    h-index

  5. MO
    Masahiro Osawa

    Okayama University, Japan

    1 publications · 15 citations

    1

    h-index

1–5 of 80

Venues

  1. Sedimentology

    5 publications · 680 citations

    5

    h-index

  2. Geology

    3 publications · 171 citations

    3

    h-index

  3. IEEE Transactions on Antennas and Propagation

    3 publications · 133 citations

    3

    h-index

  4. Journal of Sedimentary Research

    JSR · 2 publications · 46 citations

    2

    h-index

  5. AAPG Bulletin

    2 publications · 60 citations

    2

    h-index

1–5