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Science (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 PerryNature Communications|October 6, 2016
Repeating microearthquake sequences interact predominantly through postseismic slipSemechah K Y Lui, Nadia LapustaProceedings 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.Proceedings of the National Academy of Sciences of the United States of America|December 17, 2021
Dynamic rupture initiation and propagation in a fluid-injection laboratory setup with diagnostics across multiple temporal scalesMarcello Gori, Vito Rubino, Ares J Rosakis, et al.Nature|August 2, 2023
The break of earthquake asperities imaged by distributed acoustic sensingJiaxuan Li, Taeho Kim, Nadia Lapusta, et al.Pageof 2