Evidence for self-similar, triangular slip distributions on earthquakes: Implications for earthquake and fault mechanics.

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Three‐dimensional earthquake sequence simulations with evolving temperature and pore pressure due to shear heating: Effect of heterogeneous hydraulic diffusivity (2010, background): “Such difference in the location of the hypocenters and areas of largest slip is also true for many earthquakes [see Manighetti et al., 2005, Figure 12].”
Earthquake ruptures with thermal weakening and the operation of major faults at low overall stress levels (2009, background): “1 mm/m for large earthquakes [Scholz, 1982; Scholz et al., 1986; Manighetti et al., 2005].”
The Estimation of Minimum-Misfit Stochastic Models from Empirical Ground-Motion Prediction Equations (2006, background): “Manighetti et al. (2005) suggest that there is a critical distance from a major asperity beyond which an earthquake does not nucleate.”
Tohoku earthquake: a surprise? (2011, background): “Slip distribution over the fault plane is highly non-uniform in a horizontal direction (Manighetti et al., 2005, 2009).”