Diapirism

Diapirism is a geological process in which a mobile, ductile subterranean material, typically salt or shale, intrudes into overlying rock layers through buoyancy-driven upward flow, forming dome-like structures known as diapirs.

161

Publications

9.7K

Citations

394

Authors

192

Institutions

Publications per year

2017–2026

17

Authors

394

  1. CJ
    Christopher J. Talbot

    Uppsala University, Sweden

    6 publications · 422 citations

    6

    h-index

  2. MP
    Martin P. A. Jackson

    Bureau of Economic Analysis, United States

    6 publications · 1.7K citations

    6

    h-index

  3. YP
    Yury Podladchikov

    University of Lausanne, Switzerland

    5 publications · 398 citations

    5

    h-index

  4. MA
    Mehran Arian

    Islamic Azad University, Science and Research Branch, Iran

    4 publications · 116 citations

    4

    h-index

  5. HK
    Hemin Koyi

    Uppsala University, Sweden

    4 publications · 120 citations

    4

    h-index

1–5 of 394

Venues

  1. Tectonophysics

    14 publications · 1.5K citations

    13

    h-index

  2. AAPG Bulletin

    13 publications · 639 citations

    11

    h-index

  3. Journal of Structural Geology

    10 publications · 774 citations

    10

    h-index

  4. Marine and Petroleum Geology

    8 publications · 1.3K citations

    8

    h-index

  5. Geological Society London Special Publications

    8 publications · 349 citations

    8

    h-index

1–5