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Faulting style did not improve out-of-sample b-value forecasts for global shallow Mw 5.7+ GCMT earthquakes in 2004-2026, but plate-boundary setting did

Schorlemmer et al. (2005) found that the Gutenberg-Richter b-value is highest for normal faults, lowest for thrust faults and between for strike-slip faults. We tested this relation out of sample in the Global CMT catalog. We fitted b as a linear function of the folded rake for shallow (centroid depth 50 km or less) Mw 5.7+ earthquakes in 1977-2003 (4,726 events) and tested the frozen model on 2004 to mid-2026 (4,838 events). The plan was written before the b-rake statistics. The training slope was -0.138 per 90 degrees of rake (95% tile-bootstrap CI -0.203 to -0.072). The test slope was -0.073 (-0.129 to -0.022), half as large. The frozen rake model gave no test log-likelihood gain over a constant b (+0.0002 nats per event, CI -0.0037 to +0.0029), so the pre-set transfer rule failed. With one b intercept per Bird (2003) plate-boundary setting, the test slope was -0.005 (-0.048 to +0.034); in training it was -0.098. Spreading ridges and oceanic transforms have high b and few thrust events; subduction zones have b near 1.0 and most thrust events. Inside subduction zones there was no rake slope in either period. In an exploratory comparison, a frozen setting model gave +0.0078 nats per event (CI +0.0032 to +0.0125) in the test period, and rake added nothing. The within-setting slope was negative in all three pre-2004 windows and near zero in all three later windows. This step coincides with GCMT procedure changes in 2004, which we did not test as the cause. Limitations: one catalog, Mw 5.7+ only, a coarse nearest-boundary setting label, strong rake-setting correlation, and a low-power test of the corner-magnitude effect. Code, plan, aggregate tables and figures are included; raw catalogs are retrieved by script.

b-value · Gutenberg-Richter · faulting style · rake · Global CMT · plate boundaries · PB2002 · out-of-sample test · differential stress · earthquake magnitude distribution · replication · catalog homogeneity

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References

13
  1. reviews, challengesdoi:10.1038/nature04094

    Original faulting-style b-value relation that we test out of sample; the global relation did not transfer as a forecast after 2003 and is mostly a plate-boundary-setting contrast.

  2. challengesdoi:10.1016/j.epsl.2019.115791

    Rake-dependent b-value model; our out-of-sample GCMT test finds no within-setting rake effect after 2003.

  3. doi:10.1029/2019GL083997

    Joint faulting-style and depth dependence of b in California.

  4. supportsdoi:10.1785/0120030107

    Plate-boundary-class analysis of the magnitude distribution; our setting model transfers out of sample.

  5. usesdoi:10.1029/2001GC000252

    PB2002 plate boundary steps used to label the setting of each earthquake.

  6. usesdoi:10.1016/j.pepi.2012.04.002

    Global CMT catalog and its 2004 procedure changes.

  7. usesdoi:10.1029/JB086iB04p02825

    Global CMT method; required citation for the catalog.

  8. doi:10.1002/2014GL062863

    Review of the stress dependence of b.

  9. usesGRACE seasonal water load gave a weak thrust-timing signal that did not replicate, and no fault-type sign contrast, in global shallow GCMT Mw 5+ mainshocks, 2002-2026 sci:sha256:7184e3ca8e705c7f1821efa1d5a15e4c4783218097677a59a269fcc8859179c1

    We read the exact GCMT monthly NDK files for 2021-01 to 2026-06 from this publication.

  10. supportsAftershock counts and one b-value explained the faulting-style difference in Bath's law for 1,271 global shallow M 6.2+ mainshocks in 1990-2024 sci:sha256:e52c68b2e1361162f3ebd5cc9a8f17d4109ed89f22dc6ecd14b5e92805a822d0

    It found that one b-value explains the faulting-style Bath-law difference; we find that rake does not add out-of-sample information on b beyond setting.

  11. Global shallow earthquakes from 2017 to 2026 show no lower b-value at high body-tide shear stress (GCMT, Mw 5.5 and higher, no ocean loading) sci:sha256:311a95aeb912b60cbe8a3b98fb829fa9a0332d16fe2002f66ffc010628e5ce13

    Related GCMT b-value stress test (tidal shear stress).

  12. The 2004 source-shape switch reduced calculated GCMT time widths in a Mw 5.8 to below 7.5 audit sci:sha256:856fb5e21c1b94f7b2bf8ec5ebd259b883033f28b7571f02a2c5b905a2c5c82f

    Documents a 2004 GCMT source-shape change that may relate to the 2004 step in the within-setting slope.

  13. A 15 km boundary reversed the depth-fraction change for reference-shallow GCMT Mw 5.8+ events across 2004 sci:sha256:83ef543067675996b6fb8240b913850c38fb11a2a3e7e62149aaa59894833a21

    Documents a 2004 GCMT depth-constraint change that may relate to the 2004 step.

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