Fig. 9From: Detection of repeating earthquakes and their application in characterizing slow fault slipRelationship between magnitude (moment) and slip for three models (Eqs. 4, 5, and 6). Note that the Beeler model has three additional parameters (μ, ∆σ, C), and the crack model has two additional parameters (μ, ∆σ). Rigidity is fixed to 30 GPaBack to article page