Dynamic Rupture Onset is a theoretical construct in seismology that identifies the precise spatiotemporal initiation phase of earthquake rupture propagation, distinguished from other nucleation stages by the transition from quasi-static weakening to self-sustaining dynamic fault slip governed by wave-mediated stress transfer.
26
Publications
1.6K
Citations
72
Authors
59
Institutions
Publications per year
2017–2026
9
Parents
Publications
26
1–5 of 26
Authors
72
- YB
5
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- BJ
2
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- SI
2
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1–5 of 72
Institutions
59
University of Southern California
Los Angeles, United States
5 h-index
5 publications
966 citations
Centre National de la Recherche Scientifique
Paris, France
4 h-index
12 publications
390 citations
Université Grenoble Alpes
Saint-Martin-d'Hères, France
3 h-index
3 publications
122 citations
Institut de Recherche pour le Développement
Marseille, France
3 h-index
3 publications
105 citations
Université Savoie Mont Blanc
Chambéry, France
2 h-index
2 publications
86 citations
Laboratoire de Physique de l'Ecole Normale Supérieure
Paris, France
2 h-index
2 publications
37 citations
Institut des Sciences de la Terre
Grenoble, France
2 h-index
2 publications
86 citations
Bureau de Recherches Géologiques et Minières
Orléans, France
2 h-index
2 publications
67 citations
1–8 of 59
Venues
- Earth and Planetary Science Letters
3 publications · 359 citations
3
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- Tectonophysics
3 publications · 119 citations
3
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- Journal of the Mechanics and Physics of Solids
3 publications · 411 citations
3
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- International Journal of Hydrogen Energy
1 publications · 21 citations
1
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- Pure and Applied Geophysics
PAGEOPH · 1 publications · 19 citations
1
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1–5