Rift Reactivation

Rift Reactivation is a tectonic process in which pre-existing rift zones within continental plates, characterized by ancient extensional fault systems and lithospheric weaknesses, experience renewed extensional, transtensional, or inversion deformation due to subsequent far-field stresses, distinguishable from primary rifting by the preferential localization of strain along earlier-formed structural discontinuities.

139

Publications

9.5K

Citations

459

Authors

225

Institutions

Publications per year

2017–2026

35

Authors

459

  1. CJ
    Christopher Jackson

    Imperial College London, United Kingdom

    5 publications · 532 citations

    5

    h-index

  2. RB
    Rebecca Bell

    Imperial College London, United Kingdom

    4 publications · 449 citations

    4

    h-index

  3. HF
    Haakon Fossen

    University of Bergen, Norway

    4 publications · 439 citations

    4

    h-index

  4. GM
    Giänreto Manatschal

    Université de Strasbourg, France

    4 publications · 566 citations

    4

    h-index

  5. SC
    Sierd Cloetingh

    Vrije Universiteit Amsterdam, Netherlands

    3 publications · 307 citations

    3

    h-index

1–5 of 459

Venues

  1. Tectonics

    19 publications · 2.4K citations

    18

    h-index

  2. Geological Society London Special Publications

    14 publications · 1.3K citations

    13

    h-index

  3. Tectonophysics

    11 publications · 1K citations

    11

    h-index

  4. Journal of the Geological Society

    JGS · 6 publications · 361 citations

    6

    h-index

  5. Basin Research

    6 publications · 247 citations

    6

    h-index

1–5