Passive Margin Inversion

Passive Margin Inversion is a tectonic process in which a previously extensional continental margin, formed during rifting and seafloor spreading, undergoes compressional reactivation due to far-field stresses, resulting in the uplift and deformation of sedimentary basins and crustal thickening along formerly passive margins.

89

Publications

5.8K

Citations

346

Authors

188

Institutions

Publications per year

2017–2026

12

Authors

346

  1. PB
    Philippe Boulvais

    Géosciences Rennes, France

    3 publications · 182 citations

    3

    h-index

  2. JB
    J. Brendan Murphy

    St. Francis Xavier University, Canada

    3 publications · 162 citations

    3

    h-index

  3. YL
    Yves Lagabrielle

    Centre National de la Recherche Scientifique, France

    3 publications · 182 citations

    3

    h-index

  4. JR
    Jean‐Claude Ringenbach

    Total (France), France

    3 publications · 163 citations

    3

    h-index

  5. CC
    Camille Clerc

    Centre National de la Recherche Scientifique, France

    3 publications · 182 citations

    3

    h-index

1–5 of 346

Venues

  1. Tectonophysics

    12 publications · 747 citations

    12

    h-index

  2. Geology

    5 publications · 348 citations

    5

    h-index

  3. Journal of Geophysical Research Atmospheres

    JGR · 5 publications · 530 citations

    5

    h-index

  4. Marine and Petroleum Geology

    4 publications · 541 citations

    4

    h-index

  5. Geological Society London Special Publications

    4 publications · 256 citations

    4

    h-index

1–5