Fault Strength Evolution

Fault Strength Evolution is the time-dependent process by which the mechanical resistance of a fault to shear slip changes due to variations in stress, frictional properties, fluid pressure, and rock damage, distinguishing it from static fault strength models by explicitly accounting for dynamic physicochemical feedbacks during the earthquake nucleation cycle.

175

Publications

14K

Citations

479

Authors

213

Institutions

Publications per year

2017–2026

41

Authors

479

  1. CM
    Chris Marone

    Pennsylvania State University, United States

    6 publications · 786 citations

    6

    h-index

  2. AN
    André Niemeijer

    Utrecht University, Netherlands

    5 publications · 418 citations

    5

    h-index

  3. GD
    Giulio Di Toro

    University of Padua, Italy

    5 publications · 349 citations

    5

    h-index

  4. TH
    Takehiro Hirose

    Japan Agency for Marine-Earth Science and Technology, Japan

    4 publications · 269 citations

    4

    h-index

  5. SB
    S. B. Nielsen

    Istituto Nazionale di Geofisica e Vulcanologia, Italy

    4 publications · 329 citations

    4

    h-index

1–5 of 479

Venues

  1. Tectonophysics

    20 publications · 1.9K citations

    16

    h-index

  2. Earth and Planetary Science Letters

    15 publications · 1.1K citations

    15

    h-index

  3. Journal of Geophysical Research Atmospheres

    JGR · 14 publications · 2.5K citations

    14

    h-index

  4. Journal of Geophysical Research Solid Earth

    15 publications · 585 citations

    14

    h-index

  5. Geology

    13 publications · 1.6K citations

    13

    h-index

1–5