Maximum Flooding Surfaces

Maximum Flooding Surface is a stratigraphic surface of marine origin that represents the most landward transgressive extent of a marine shoreline, distinguished from other sequence boundaries by marking the culmination of relative sea-level rise and the transition from retrogradational to progradational stacking patterns within a depositional sequence.

82

Publications

4.8K

Citations

242

Authors

123

Institutions

Publications per year

2017–2026

12

Authors

242

  1. OC
    Octavian Catuneanu

    University of Alberta, Canada

    4 publications · 191 citations

    4

    h-index

  2. XL
    Xue Liangqing

    The University of Texas at Austin, United States

    3 publications · 131 citations

    3

    h-index

  3. MA
    Mark A. Partington

    BP (United Kingdom), United Kingdom

    3 publications · 595 citations

    3

    h-index

  4. JR
    John R. Underhill

    University of Edinburgh, United Kingdom

    3 publications · 595 citations

    3

    h-index

  5. WE
    William E. Galloway

    The University of Texas at Austin, United States

    3 publications · 1.1K citations

    3

    h-index

1–5 of 242

Venues

  1. Geological Society London Special Publications

    11 publications · 399 citations

    10

    h-index

  2. AAPG Bulletin

    8 publications · 1.5K citations

    8

    h-index

  3. Geological Society London Petroleum Geology Conference series

    Conference · 7 publications · 658 citations

    7

    h-index

  4. Journal of Sedimentary Research

    JSR · 5 publications · 374 citations

    5

    h-index

  5. Sedimentology

    3 publications · 148 citations

    3

    h-index

1–5