TY - JOUR
T1 - Rupture Jumping and Seismic Complexity in Models of Earthquake Cycles for Fault Stepovers with Off-Fault Plasticity
AU - Mia, Md Shumon
AU - Abdelmeguid, Mohamed
AU - Harris, Ruth A.
AU - Elbanna, Ahmed E.
N1 - The authors acknowledge support from the Southern California Earthquake Center through a collaborative agreement between National Science Foundation (NSF) Grant Number EAR0529922 and U.S. Geological Survey (USGS) Grant Number 07HQAG0008 and the National Science Foundation CAREER Award Number 1753249 for modeling complex fault zone structures. This material is also based upon work partially supported by the Department of Energy under Award Number DE-FE0031685 to investigate spatiotemporal complexity of induced earthquakes. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government.
PY - 2024/6
Y1 - 2024/6
N2 - Fault stepovers are prime examples of geometric complexity in natural fault zones that may affect seismic hazard by determining whether an earthquake rupture continues propagating or abruptly stops. However, the long-term pattern of seismicity near-fault stepovers and underlying mechanisms of rupture jumping in the context of earthquake cycles are rarely studied. Leveraging a hybrid numerical scheme combining the finite element and the spectral boundary integral methods, FEBE, we carry out fully dynamic simulations of sequences of earthquakes and aseismic slip for both compressive and tensile stepovers with off-fault plasticity. We consider a rate-and-state friction law for the fault friction and pressure-sensitive Drucker–Prager plasticity for the off-fault bulk response. We observe that the accumulation of plastic deformation, an indication of off-fault damage, is significantly different in the two cases, with more plastic deformation projected in the overlapping region for the tensile stepover. The seismic pattern for a tensile stepover is more complex than for a compressive stepover, and incorporating plasticity also increases complexity, relative to the elastic case. A tensile stepover with off-fault plasticity shows rupture segmentation, temporal clustering, and frequent rupture jumping from one fault to another. These results shed light on possible mechanisms of rupture jumping in fault stepovers as well as the long-term evolution of the fault zone.
AB - Fault stepovers are prime examples of geometric complexity in natural fault zones that may affect seismic hazard by determining whether an earthquake rupture continues propagating or abruptly stops. However, the long-term pattern of seismicity near-fault stepovers and underlying mechanisms of rupture jumping in the context of earthquake cycles are rarely studied. Leveraging a hybrid numerical scheme combining the finite element and the spectral boundary integral methods, FEBE, we carry out fully dynamic simulations of sequences of earthquakes and aseismic slip for both compressive and tensile stepovers with off-fault plasticity. We consider a rate-and-state friction law for the fault friction and pressure-sensitive Drucker–Prager plasticity for the off-fault bulk response. We observe that the accumulation of plastic deformation, an indication of off-fault damage, is significantly different in the two cases, with more plastic deformation projected in the overlapping region for the tensile stepover. The seismic pattern for a tensile stepover is more complex than for a compressive stepover, and incorporating plasticity also increases complexity, relative to the elastic case. A tensile stepover with off-fault plasticity shows rupture segmentation, temporal clustering, and frequent rupture jumping from one fault to another. These results shed light on possible mechanisms of rupture jumping in fault stepovers as well as the long-term evolution of the fault zone.
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U2 - 10.1785/0120230249
DO - 10.1785/0120230249
M3 - Article
AN - SCOPUS:85195554488
SN - 0037-1106
VL - 114
SP - 1466
EP - 1480
JO - Bulletin of the Seismological Society of America
JF - Bulletin of the Seismological Society of America
IS - 3
ER -