1. Ambraseys N. N. (1969). Maximum intensity of ground movements caused by faulting Proceedings Fourth World Conference on Earthquake Engineering Santiago Chile January. 9
2. DJIOGANG etal
3. A fault constitutive relation accounting for thermal pressurization of pore fluid;Andrews D. J.;J. Geophys. Res. 105 (B12). Doi,2002
4. Effect of fluid circulation on subduction interface tectonic processes : Insights from thermo-mechanical numerical modelling;Angiboust S.;Earth and Planetary Science Letters,2012
5. What can physical source models tell us about the recurrence time of earthquakes. Earth Sci;Bizzarri A.;Rev.,2012