Geological Connectivity

Geological Connectivity is the degree to which subsurface geological elements are physically linked through continuous pathways that enable fluid flow, distinguished from other connectivity types by its dependence on static rock properties, stratigraphic architecture, and structural configurations.

196

Publications

12.4K

Citations

544

Authors

251

Institutions

Publications per year

2017–2026

29

Authors

544

  1. RE
    R. E. Holdsworth

    Durham University, United Kingdom

    3 publications · 269 citations

    3

    h-index

  2. KM
    Ken McCaffrey

    Durham University, United Kingdom

    3 publications · 139 citations

    3

    h-index

  3. SJ
    S. J. Webb

    University of the Witwatersrand, South Africa

    2 publications · 111 citations

    2

    h-index

  4. AD
    Athol D. Abrahams

    University at Buffalo, State University of New York, United States

    2 publications · 55 citations

    2

    h-index

  5. JV
    J.J. Veevers

    Macquarie University, Australia

    2 publications · 192 citations

    2

    h-index

1–5 of 544

Venues

  1. Geology

    44 publications · 4.4K citations

    33

    h-index

  2. Geological Society of America Bulletin

    40 publications · 2.2K citations

    24

    h-index

  3. South African Journal of Geology

    SAJG · 7 publications · 391 citations

    7

    h-index

  4. AAPG Bulletin

    6 publications · 107 citations

    6

    h-index

  5. Geological Society London Special Publications

    5 publications · 169 citations

    5

    h-index

1–5