Earthquake Rupture in Fault Zones With Along‐Strike Material Heterogeneity
Huang, Yihe
2018-11
Citation
Huang, Yihe (2018). "Earthquake Rupture in Fault Zones With Along‐Strike Material Heterogeneity." Journal of Geophysical Research: Solid Earth 123(11): 9884-9898.
Abstract
Geological and geophysical observations reveal along‐strike fault zone heterogeneity on major strike‐slip faults, which can play a significant role in earthquake rupture propagation and termination. I present 2‐D dynamic rupture simulations to demonstrate rupture characteristics in such heterogeneous fault zone structure. The modeled rupture is nucleated in a damaged fault zone and propagates on a preexisting fault toward the zone of intact rocks. There is an intermediate range of nucleation lengths that only allow rupture to spontaneously propagate in the damaged fault zone but not in a homogeneous medium given the same stresses and frictional parameters. Rupture with an intermediate nucleation length tends to stop when it reaches the zone of intact rocks for uniform fault stress conditions, especially when the rupture propagation distance in the damaged fault zone is relatively short and when the damaged fault zone is relatively narrow or smooth in the fault‐normal direction. Pronounced small‐scale heterogeneity within the damaged fault zone also contributes to such early rupture termination. In asymmetric fault zones bisected by a bimaterial fault, rupture moving in the direction of slip of faster rocks tends to terminate under the same conditions as in symmetric fault zones, whereas rupture moving in the direction of slip of slower rocks can penetrate into the zone of intact rocks. A sufficiently large asperity located at the edge of the zone of intact rocks also allows break‐through rupture. The results suggest that the along‐strike fault zone heterogeneity can play a critical role in seismicity distribution.Plain Language SummaryNatural faults are surrounded by a zone of deformed rocks to accommodate strain localization. Such fault zone is not continuous along the fault, but rather includes segments of relatively damaged rocks adjacent to segments of relatively intact rocks. By simulating the dynamic interactions between fault stress, friction, and fault zone heterogeneities during the earthquake rupture process, I show that rupture is more likely to spontaneously propagate inside the damaged fault zone and stop when it reaches the relatively intact zone for uniform fault stress conditions. This phenomenon is less pronounced when the damaged fault zone becomes wider, sharper, and more damaged, indicating a higher likelihood of having large earthquakes that can penetrate into the relatively intact zone on more mature faults. The results suggest that a priori knowledge of the fault zone heterogeneity is critical for understanding the spatial distribution of earthquakes and the likelihood of having large earthquakes.Key PointsRupture nucleated in a damaged fault zone tends to terminate when it propagates along strike to an intact zone for uniform fault stressesRupture tends to penetrate into the relatively intact zone when the damaged fault zone becomes wider, sharper, and more damagedAn asperity at the edge of the relatively intact zone can facilitate rupture when its size is comparable to the nucleation half‐lengthPublisher
John Wiley & Sons, Inc.
ISSN
2169-9313 2169-9356
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