More Like this

1. Microscopic model for the stacking-fault potential and the exciton wave function in GaAs

   https://doi.org/10.1103/PhysRevB.101.125420  

   Durnev, Mikhail V. ; Glazov, Mikhail M. ; Linpeng, Xiayu ; Viitaniemi, Maria L. ; Matthews, Bethany ; Spurgeon, Steven R. ; Sushko, Peter V. ; Wieck, Andreas D. ; Ludwig, Arne ; Fu, Kai-Mei C. ( March 2020 , Physical Review B)
2. The damage is done: Low fault friction recorded in the damage zone of the shallow Japan Trench décollement

   https://doi.org/10.1002/2015JB012311  

   Keren, Tucker T. ; Kirkpatrick, James D. ( May 2016 , Journal of Geophysical Research: Solid Earth)
3. Quartz fluid inclusion abundance and off-fault damage in a deeply exhumed, strike-slip, seismogenic fault

   https://doi.org/10.1016/j.jsg.2020.104118  

   Song, Won Joon ; Johnson, Scott E. ; Gerbi, Christopher C. ( June 2020 , Journal of Structural Geology)
4. DYNAMIC FRACTURING IN FAULT TIP DAMAGE ZONES? AN OUTCROP STUDY OF THE SEVIER FAULT ZONE, SOUTHERN UTAH

   https://doi.org/10.1130/abs/2022AM-377982  

   Surpless, Benjamin ; McKeighan, Caroline ( January 2022 , Geological Society of America Abstracts with Programs)
5. Dueling dynamics of low-angle normal fault rupture with splay faulting and off-fault damage

   https://doi.org/10.1038/s41467-023-37063-1  

   Biemiller, J. ; Gabriel, A.-A. ; Ulrich, T. ( December 2023 , Nature Communications)

   Abstract Despite a lack of modern large earthquakes on shallowly dipping normal faults, Holocene M w  > 7 low-angle normal fault (LANF; dip<30°) ruptures are preserved paleoseismically and inferred from historical earthquake and tsunami accounts. Even in well-recorded megathrust earthquakes, the effects of non-linear off-fault plasticity and dynamically reactivated splay faults on shallow deformation and surface displacements, and thus hazard, remain elusive. We develop data-constrained 3D dynamic rupture models of the active Mai’iu LANF that highlight how multiple dynamic shallow deformation mechanisms compete during large LANF earthquakes. We show that shallowly-dipping synthetic splays host more coseismic slip and limit shallow LANF rupture more than steeper antithetic splays. Inelastic hanging-wall yielding localizes into subplanar shear bands indicative of newly initiated splay faults, most prominently above LANFs with thick sedimentary basins. Dynamic splay faulting and sediment failure limit shallow LANF rupture, modulating coseismic subsidence patterns, near-shore slip velocities, and the seismic and tsunami hazards posed by LANF earthquakes. 

   more » « less