Oblique Rifting

Oblique Rifting is a tectonic process in which continental or oceanic extension occurs at an angle to the dominant plate boundary or rift trend, distinguished from orthogonal rifting by the significant component of shear stress accompanying divergence.

119

Publications

9.4K

Citations

407

Authors

198

Institutions

Publications per year

2017–2026

16

Authors

407

  1. NB
    Nicolas Bellahsen

    Sorbonne Université, France

    6 publications · 567 citations

    6

    h-index

  2. SL
    Sylvie Leroy

    Sorbonne Université, France

    6 publications · 562 citations

    6

    h-index

  3. ED
    Elia d’Acremont

    Sorbonne Université, France

    5 publications · 484 citations

    5

    h-index

  4. PJ
    Paul J. Umhoefer

    Northern Arizona University, United States

    4 publications · 176 citations

    4

    h-index

  5. JA
    Julia Autin

    Centre National de la Recherche Scientifique, France

    4 publications · 354 citations

    4

    h-index

1–5 of 407

Venues

  1. Tectonophysics

    21 publications · 2.2K citations

    20

    h-index

  2. Tectonics

    9 publications · 793 citations

    9

    h-index

  3. Geochemistry Geophysics Geosystems

    8 publications · 631 citations

    8

    h-index

  4. Geological Society London Special Publications

    6 publications · 395 citations

    6

    h-index

  5. Journal of Geophysical Research Atmospheres

    JGR · 5 publications · 559 citations

    5

    h-index

1–5