Time-dependent Fault Strength

Time-Dependent Fault Strength is a geomechanical property representing the progressive evolution of a fault's resistance to shear failure over time due to post-seismic healing, creep, and interseismic stress accumulation, distinguishing it from instantaneous or static measures of fault strength by explicitly incorporating temporal variations in frictional and cohesive behavior along fault zones.

23

Publications

1.3K

Citations

67

Authors

47

Institutions

Publications per year

2017–2026

5

Authors

67

  1. MJ
    Matt J. Ikari

    University of Bremen, Germany

    2 publications · 153 citations

    2

    h-index

  2. MV
    Martijn van den Ende

    Observatoire de la Côte d’Azur, France

    2 publications · 53 citations

    2

    h-index

  3. AN
    André Niemeijer

    Utrecht University, Netherlands

    2 publications · 53 citations

    2

    h-index

  4. BM
    B. M. Carpenter

    University of Oklahoma, United States

    2 publications · 153 citations

    2

    h-index

  5. MH
    Moritz Heimpel

    University of Alberta, Canada

    1 publications · 38 citations

    1

    h-index

1–5 of 67

Venues

  1. Earth and Planetary Science Letters

    4 publications · 189 citations

    4

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 3 publications · 201 citations

    3

    h-index

  3. Journal of Geophysical Research Solid Earth

    3 publications · 212 citations

    3

    h-index

  4. Pure and Applied Geophysics

    PAGEOPH · 2 publications · 265 citations

    2

    h-index

  5. Geomorphology

    1 publications · 45 citations

    1

    h-index

1–5