Continental Transform Faults

Continental Transform Faults is a geologic fault that serves as a tectonic boundary where two continental plates slide horizontally past each other within the Earth's lithosphere, distinguished by strike-slip motion and the absence of active volcanism typical of divergent or convergent boundaries.

352

Publications

35.7K

Citations

934

Authors

369

Institutions

Publications per year

2017–2026

46

Authors

934

  1. RG
    Richard G. Gordon

    Rice University, United States

    9 publications · 4.5K citations

    9

    h-index

  2. ZB
    Zvi Ben‐Avraham

    Tel Aviv University, Israel

    8 publications · 447 citations

    8

    h-index

  3. RC
    R. C. Searle

    Durham University, United Kingdom

    8 publications · 453 citations

    8

    h-index

  4. CD
    Charles DeMets

    University of Wisconsin–Madison, United States

    7 publications · 4.4K citations

    7

    h-index

  5. TG
    Taras Gerya

    ETH Zurich, Switzerland

    6 publications · 392 citations

    6

    h-index

1–5 of 934

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 60 publications · 7.8K citations

    43

    h-index

  2. Geophysical Journal International

    GJI · 21 publications · 6.4K citations

    19

    h-index

  3. Geology

    17 publications · 1.7K citations

    17

    h-index

  4. Geochemistry Geophysics Geosystems

    18 publications · 1K citations

    16

    h-index

  5. Tectonics

    19 publications · 1.1K citations

    16

    h-index

1–5