Finite-fault Source Effects

Finite-Fault Source Effects is a seismological construct that characterizes the spatial and temporal heterogeneity of rupture propagation across an extended fault plane during an earthquake, distinguishing it from point-source representations by accounting for variations in slip magnitude, timing, and direction over finite fault dimensions.

37

Publications

6.5K

Citations

104

Authors

46

Institutions

Publications per year

2017–2026

5

Authors

104

  1. JW
    J. Woessner

    ETH Zurich, Switzerland

    3 publications · 217 citations

    3

    h-index

  2. KB
    K. B. Olsen

    San Diego State University, United States

    2 publications · 44 citations

    2

    h-index

  3. QH
    Qinghua Huang

    Peking University, China

    2 publications · 58 citations

    2

    h-index

  4. SW
    Stefan Wiemer

    ETH Zurich, Switzerland

    2 publications · 183 citations

    2

    h-index

  5. HR
    Hengxin Ren

    Peking University, China

    2 publications · 58 citations

    2

    h-index

1–5 of 104

Venues

  1. Bulletin of the Seismological Society of America

    BSSA · 14 publications · 4.8K citations

    14

    h-index

  2. Geophysical Research Letters

    5 publications · 281 citations

    5

    h-index

  3. Geophysical Journal International

    GJI · 3 publications · 73 citations

    3

    h-index

  4. Journal of Geophysical Research Atmospheres

    JGR · 3 publications · 217 citations

    3

    h-index

  5. Seismological Research Letters

    SRL · 2 publications · 107 citations

    2

    h-index

1–5