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Nature Communications|October 6, 2016
Repeating microearthquake sequences interact predominantly through postseismic slipSemechah K Y Lui, Nadia LapustaScientific Reports|December 3, 2022
Interdependent effects of fluid injection parameters on triggered aseismic slip and seismicityRiddhi Mandal, Semechah K Y LuiScientific Reports|November 20, 2024
Insights on earthquake nucleation revealed by numerical simulation and unsupervised machine learning of laboratory-scale earthquakeSheng Hua Ye, Semechah K Y Lui, R Paul YoungScience (New York, N.Y.)|June 11, 2016
Deeper penetration of large earthquakes on seismically quiescent faultsJunle Jiang, Nadia LapustaNature|January 11, 2013
Stable creeping fault segments can become destructive as a result of dynamic weakeningHiroyuki Noda, Nadia LapustaNature|March 11, 2021
Propagation of large earthquakes as self-healing pulses or mild cracksValère Lambert, Nadia Lapusta, Stephen PerryProceedings of the National Academy of Sciences of the United States of America|November 21, 2007
Pulse-like and crack-like ruptures in experiments mimicking crustal earthquakesXiao Lu, Nadia Lapusta, Ares J RosakisScience (New York, N.Y.)|May 15, 2012
Under the hood of the earthquake machine: toward predictive modeling of the seismic cycleSylvain Barbot, Nadia Lapusta, Jean-Philippe AvouacNature Communications|January 18, 2022
Fault rock heterogeneity can produce fault weakness and reduce fault stabilityJohn D Bedford, Daniel R Faulkner, Nadia LapustaProceedings of the National Academy of Sciences of the United States of America|August 21, 2020
Illuminating the physics of dynamic friction through laboratory earthquakes on thrust faultsYuval Tal, Vito Rubino, Ares J Rosakis, et al.Pageof 2