Stratigraphic Unconformities

Stratigraphic Unconformity is a surface bounding two strata or rock units that represents a gap in the geological record due to a period of erosion or non-deposition, distinguishing it from other stratigraphic contacts by indicating a significant hiatus in sedimentation.

140

Publications

10.9K

Citations

300

Authors

131

Institutions

Publications per year

2017–2026

14

Authors

300

  1. NC
    Nicholas Christie‐Blick

    Lamont-Doherty Earth Observatory, United States

    3 publications · 179 citations

    3

    h-index

  2. PR
    Peter R. Vail

    Rice University, United States

    3 publications · 893 citations

    3

    h-index

  3. WB
    W. B. Harland

    Sedgwick Museum of Earth Sciences, United Kingdom

    2 publications · 35 citations

    2

    h-index

  4. BG
    Bruno Granier

    Université de Bretagne Occidentale, France

    2 publications · 43 citations

    2

    h-index

  5. CP
    Chris Paola

    University of Minnesota, United States

    2 publications · 700 citations

    2

    h-index

1–5 of 300

Venues

  1. AAPG Bulletin

    17 publications · 3.5K citations

    13

    h-index

  2. Canadian Journal of Earth Sciences

    6 publications · 220 citations

    6

    h-index

  3. Sedimentary Geology

    5 publications · 340 citations

    5

    h-index

  4. Geological Society of America Bulletin

    5 publications · 373 citations

    5

    h-index

  5. Journal of Sedimentary Research

    JSR · 5 publications · 292 citations

    5

    h-index

1–5