Canyon-flank Instability

Canyon-Flank Instability is a geological phenomenon characterized by the progressive weakening and failure of submarine slope materials along the margins of underwater canyons, distinguished from other forms of seafloor instability by its confinement to canyon wall environments and its sensitivity to sediment overloading, fluid migration, and topographically induced stress concentration.

13

Publications

782

Citations

39

Authors

38

Institutions

Publications per year

2017–2026

1

Authors

39

  1. AG
    Andrew Green

    University of KwaZulu-Natal, South Africa

    1 publications · 27 citations

    1

    h-index

  2. MA
    Mohammad Adampira

    Islamic Azad University, Science and Research Branch, Iran

    1 publications · 48 citations

    1

    h-index

  3. RJ
    Robert J. Poreda

    University of Rochester, United States

    1 publications · 62 citations

    1

    h-index

  4. DR
    Donald R. Lowe

    Stanford University, United States

    1 publications · 192 citations

    1

    h-index

  5. WR
    William R. Bryant

    Texas A&M University, United States

    1 publications · 63 citations

    1

    h-index

1–5 of 39

Venues

  1. Geology

    2 publications · 75 citations

    2

    h-index

  2. Icarus

    1 publications · 107 citations

    1

    h-index

  3. Quaternary International

    1 publications · 11 citations

    1

    h-index

  4. Journal of Volcanology and Geothermal Research

    1 publications · 162 citations

    1

    h-index

  5. AAPG Bulletin

    1 publications · 63 citations

    1

    h-index

1–5