Splay Faulting

Splay Faulting is a structural geologic process characterized by the formation of secondary thrust faults branching from a main subduction megathrust, which accommodate differential strain partitioning along the plate boundary.

92

Publications

4.7K

Citations

354

Authors

195

Institutions

Publications per year

2017–2026

30

Authors

354

  1. PJ
    Peter J. Haeussler

    United States Geological Survey, United States

    4 publications · 95 citations

    4

    h-index

  2. GK
    Gaku Kimura

    The University of Tokyo, Japan

    4 publications · 471 citations

    4

    h-index

  3. LM
    Lee M. Liberty

    Boise State University, United States

    4 publications · 95 citations

    4

    h-index

  4. YK
    Yoshiyuki Kaneda

    Japan Agency for Marine-Earth Science and Technology, Japan

    3 publications · 823 citations

    3

    h-index

  5. RV
    Roland von Huene

    United States Geological Survey, United States

    3 publications · 69 citations

    3

    h-index

1–5 of 354

Venues

  1. Geophysical Research Letters

    9 publications · 579 citations

    9

    h-index

  2. Tectonophysics

    6 publications · 309 citations

    6

    h-index

  3. Geochemistry Geophysics Geosystems

    5 publications · 310 citations

    5

    h-index

  4. Earth and Planetary Science Letters

    4 publications · 186 citations

    4

    h-index

  5. New Zealand Journal of Geology and Geophysics

    NZJG · 4 publications · 71 citations

    4

    h-index

1–5