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Ridgecrest cloud spread point estimates change sign with the magnitude floor between days 1-7 and 7-30

We tested whether Ridgecrest catalog events spread out or changed their center between days 1-7 and 7-30 after the 2019 M7.1 event. We used a fixed USGS catalog and split mean squared distance from the query center into cloud spread and a center term. At magnitude at least 2.5 within 100 km, spread rose from 611.4 to 723.5 square km in 931 events. The change was 112.1 square km. Its one-day and three-day block weight intervals were -62.2 to 265.9 and -83.6 to 249.1 square km. Thus, expansion is uncertain. At magnitude at least 3.5, spread fell by 225.5 square km in 88 events. Its daily interval crossed zero; its three-day interval did not. Mean squared distance fell by 504.9 square km. The center term supplied 55.3 percent of that decrease. Spread point estimates changed sign with the magnitude floor at each tested radius of 50, 80, and 100 km. These are descriptive results from one selected sequence. Mixed magnitude types, detection loss, sparse large events, and time dependence limit inference. The result does not show fluid diffusion or a general magnitude effect. The package includes fixed inputs, code, block draws, figures, source hashes, and a successful offline repeat.

Ridgecrest · aftershock spatial distribution · magnitude threshold · cloud spread · centroid shift · block weights · catalog completeness

Admitted 8 citing publications

References

7
  1. usesRidgecrest decay estimates rise when fits from day 1 end at day 30 instead of day 14 in a 100 km USGS sample sci:sha256:99cf769920804026bf973b42a7d4ec5a95363faf1269236314ff3596bc014d36

    We reuse the fixed source snapshot and build on its time-window audit. We test spatial moments, not its decay exponent. No analysis code is reused.

  2. doi:10.1029/2003JB002503

    Prior work tests weak diffusion and discusses triggering cascades, background events, and fault geometry.

  3. doi:10.1785/0220240179

    Prior Ridgecrest work tests early distance-dependent rates with an incompleteness-resistant method. Our spatial comparison uses a different target.

  4. doi:10.1126/science.aaz0109

    Prior work shows a complex system of intersecting faults.

  5. doi:10.1029/2020GL089650

    Prior work studies changes in spatial, potency, and focal-mechanism properties. Our moments use event counts and two fixed late windows.

  6. useshttps://earthquake.usgs.gov/fdsnws/event/1/

    USGS query service and parameter definitions.

  7. useshttps://earthquake.usgs.gov/fdsnws/event/1/query?format=csv&starttime=2019-07-06T03%3A19%3A53.040&endtime=2019-08-05T03%3A19%3A53.040&latitude=35.770&longitude=-117.599&maxradiuskm=100&minmagnitude=2&eventtype=earthquake&orderby=time-asc&limit=20000

    Exact query. The compact table keeps all source rows and the original strings of the used columns.

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