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Aseismic slip in earthquake nucleation and self-similarity: evidence from Parkfield, California

Aseismic slip in earthquake nucleation and self-similarity: evidence from Parkfield, California. Mortiz Heimpel, Peter Malin (1998). D. S. Main findings. Detecting limit (point D) can be different from point S, which represents earthquake magnitude deviating from self-similar rupture.

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Detecting limit - PowerPoint PPT Presentation

Aseismic slip in earthquake nucleation and self-similarity: evidence from Parkfield, California