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• W2324562296 abstract "Research Article| October 01, 2013 Energy Flux of Propagating Ruptures with Cohesive Force Andrea Bizzarri Andrea Bizzarri Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Bologna, Via Donato Creti, 12, 40128 Bologna, Italybizzarri@bo.ingv.it Search for other works by this author on: GSW Google Scholar Author and Article Information Andrea Bizzarri Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Bologna, Via Donato Creti, 12, 40128 Bologna, Italybizzarri@bo.ingv.it Publisher: Seismological Society of America First Online: 14 Jul 2017 Online ISSN: 1943-3573 Print ISSN: 0037-1106 Bulletin of the Seismological Society of America (2013) 103 (5): 2670–2679. https://doi.org/10.1785/0120120335 Article history First Online: 14 Jul 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Andrea Bizzarri; Energy Flux of Propagating Ruptures with Cohesive Force. Bulletin of the Seismological Society of America 2013;; 103 (5): 2670–2679. doi: https://doi.org/10.1785/0120120335 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyBulletin of the Seismological Society of America Search Advanced Search Abstract The energy flux F at the rupture tip has been previously computed only for 2D steady‐state singular cracks. In this paper, I compute F for fully dynamic 3D ruptures, propagating both with constant and variable rupture speed (vr) over finite faults directed by a governing law with a cohesive zone (and thus nonsingular ruptures). The results presented here indicate that F is positive and increasing over the whole range of vr from zero up to P‐wave speed. This is in contrast with 2D steady‐state singular cracks, which predict the existence of a forbidden zone in the range of rupture speeds because in that interval F would be negative. Moreover, I found that in 3D ruptures with cohesive force, F is proportional to vr, again in contrast to 2D steady‐state singular cracks, in which F is not a unique function of vr and also exhibits an inverse dependence on vr. More specifically, it emerges that fast earthquakes tend to have a higher energy flux at the crack tip compared with slow ruptures. Finally, I show that the magnitude of F is basically due to its component aligned in the direction of the initial shear stress. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2324562296 title "Energy Flux of Propagating Ruptures with Cohesive Force" @default.
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