Source Rupture Complexity

Source Rupture Complexity is a seismological construct that characterizes the degree of spatial and temporal heterogeneity in the fault rupture process during an earthquake, distinguishing it from simpler, more uniform rupture models by quantifying deviations in slip distribution, propagation dynamics, and energy release patterns.

40

Publications

2.1K

Citations

110

Authors

58

Institutions

Publications per year

2017–2026

11

Authors

110

  1. HK
    Hiroo Kanamori

    California Institute of Technology, United States

    5 publications · 250 citations

    5

    h-index

  2. TL
    Thorne Lay

    University of California, Santa Cruz, United States

    3 publications · 331 citations

    3

    h-index

  3. KM
    Karen McNally

    University of California, Santa Cruz, United States

    2 publications · 57 citations

    2

    h-index

  4. NA
    Nicola Alessandro Pino

    Istituto Nazionale di Geofisica e Vulcanologia, Italy

    2 publications · 68 citations

    2

    h-index

  5. JA
    Jean‐Paul Ampuero

    California Institute of Technology, United States

    2 publications · 559 citations

    2

    h-index

1–5 of 110

Venues

  1. Bulletin of the Seismological Society of America

    BSSA · 8 publications · 282 citations

    8

    h-index

  2. Geophysical Research Letters

    7 publications · 710 citations

    7

    h-index

  3. Journal of Geophysical Research Atmospheres

    JGR · 5 publications · 268 citations

    5

    h-index

  4. Geophysical Journal International

    GJI · 4 publications · 117 citations

    4

    h-index

  5. Journal of Geophysical Research Solid Earth

    3 publications · 158 citations

    3

    h-index

1–5