Oblique Faulting

Oblique Faulting is a type of lithospheric deformation characterized by fault displacement that occurs at an angle to both the dip and strike directions of the fault plane, involving simultaneous normal or reverse and strike-slip shear components, thereby distinguishing it from purely dip-slip or strike-slip faulting mechanisms.

105

Publications

8.8K

Citations

365

Authors

169

Institutions

Publications per year

2017–2026

19

Variants

Oblique-slip Faulting

Authors

365

  1. JJ
    James Jackson

    University of Cambridge, United Kingdom

    3 publications · 493 citations

    3

    h-index

  2. AA
    Atilla Aydin

    Stanford University, United States

    3 publications · 191 citations

    3

    h-index

  3. JC
    Jean‐Yves Collot

    Institut de Recherche pour le Développement, France

    2 publications · 45 citations

    2

    h-index

  4. KP
    Keith Priestley

    University of Cambridge, United Kingdom

    2 publications · 349 citations

    2

    h-index

  5. FA
    Fabrizio Agosta

    University of Basilicata, Italy

    2 publications · 169 citations

    2

    h-index

1–5 of 365

Venues

  1. Journal of Structural Geology

    9 publications · 591 citations

    9

    h-index

  2. Tectonics

    7 publications · 400 citations

    7

    h-index

  3. AAPG Bulletin

    6 publications · 604 citations

    6

    h-index

  4. Tectonophysics

    6 publications · 194 citations

    6

    h-index

  5. Journal of Geophysical Research Atmospheres

    JGR · 6 publications · 1.4K citations

    6

    h-index

1–5