Monday Afternoon 2
Time	Session	Location	Title
1600	S14B	MW 3010	Insights From Combined Laboratory and Theoretical Investigations of Earthquake Rupture and Aseismic Fault Slip IV (joint with MR, T) Presiding: Y Fialko, University of California, San Diego; N Lapusta, California Institute of Technology; A Rosakis, California Institute of Technology    [Abstracts]
1600	S14B-01	MW 3010	Is the Chrystalls Beach Accretionary Melange a Fossil Subduction Channel Shear Zone? *A Fagereng, R H Sibson    [details]
1615	S14B-02	MW 3010	Influence of Rupture Speed on Effective Normal Stress Changes During Slip Between Dissimilar Poroelastic Materials *E M Dunham, J R Rice    [details]
1630	S14B-03	MW 3010	Asymmetric pulse-like rupture at bimaterial interface with slip-weakening friction model *L A Dalguer Dr., S M Day    [details]
1645	S14B-04	MW 3010	Normal Stress and Gaps in Interacting Strike-Slip Faults *D D Oglesby    [details]
1700	S14B-05	MW 3010	Segmentation and Maturity of Long-Term Faults Control Earthquake Slip-Length Scaling *I Manighetti, M Campillo, F Cotton, P Billion    [details]
1715	S14B-06	MW 3010	Slip-Length Scaling in Large Earthquakes: The Role of Deep Penetrating Slip Below the Seismogenic Layer *B E Shaw, S G Wesnousky    [details]
1730	S14B-07	MW 3010	Exploring the Relationship Between Early Rupture History and Final Earthquake Size *G Wurman, D D Oglesby, R M Allen    [details]
1745	S14B-08	MW 3010	Correlations and Non-predictability in the Time Evolution of Earthquake Ruptures *J E Elkhoury, L Knopoff    [details]