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Scripts from: Nonlocal dissipation far from the rupture tip affects both rupture dynamics and arrest

dc.contributor.authorBasu, Dibya Jyoti
dc.contributor.authorKe, Chun-Yu
dc.contributor.authorKammer, David S.
dc.contributor.authorMcLaskey, Gregory C.
dc.date.accessioned2025-10-01T01:25:02Z
dc.date.available2025-10-01T01:25:02Z
dc.date.issued2025-09
dc.descriptionPlease cite as: Basu, D. J., Ke, C.-Y., Kammer, D., & McLaskey, G. (2025). Scripts from: Nonlocal dissipation far from the rupture tip affects both rupture dynamics and arrest. Cornell University Library eCommons Repository. https://doi.org/10.7298/D5GP-8013
dc.description.abstractThese files are from the numerical simulations conducted in Basu et al., "Nonlocal dissipation far from the rupture tip affects both rupture dynamics and arrest" We found: Linear elastic fracture mechanics is useful for understanding earthquake rupture, but seismological evidence suggests earthquake fracture energy spanning from 1 J/m2 to 10 MJ/m2. Fracture energy is localized to the rupture tip, so high seismological estimates should instead be considered breakdown work Wb, which includes nonlocal energy dissipation, possibly arising from long-tailed secondary weakening (LTSW) that scales with final slip. However, it is unclear if LTSW and associated large Wb causes earthquakes to rupture faster and grow larger or propagate more slowly and arrest easily. We report numerical models of dynamic rupture that illuminate effects of LTSW on rupture propagation and arrest due to heterogeneous initial stress. Our findings indicate that secondary weakening always leads to a higher rupture speed and a larger rupture extent compared to scenarios without it. Additional stress drop associated with secondary weakening does more to “fuel” rupture than larger Wb does to arrest rupture.
dc.description.sponsorshipThis work was sponsored by US National Science Foundation Grant EAR‐2240375, National Science and Technology Council, Taiwan (NSTC 113-2116-M-002-031-MY3), and the Yushan Fellow Program of the Ministry of Education (MOE), Taiwan (NTU-113V1045-1)
dc.identifier.doihttps://doi.org/10.7298/d5gp-8013
dc.identifier.urihttps://hdl.handle.net/1813/117775
dc.rightsCC0 1.0 Universalen
dc.rights.urihttp://creativecommons.org/publicdomain/zero/1.0/
dc.titleScripts from: Nonlocal dissipation far from the rupture tip affects both rupture dynamics and arrest
dc.typedataset

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