1. Pre‐Existing Off‐Fault Damage Can Impede Coseismic On‐Fault Slip.
- Author
-
Wu, C. H., Cui, P., Klinger, Y., Tan, X. B., Yi, S. J., and Li, Y. S.
- Subjects
FAULT zones ,EARTHQUAKE zones ,EARTHQUAKES ,ENERGY dissipation ,FIELD research ,TSUNAMI warning systems - Abstract
Primarily due to the scarce direct field evidence along a same fault, understanding the relationship between the pre‐existing off‐fault damage and coseismic slip distribution remains challenging. This study offers the first field‐based quantitative assessments of fault damage zones along the surface rupture generated by the 2008 Mw 7.9 Wenchuan earthquake in China over eight profiles with 254 outcrops. The width and mean tectonic fracture intensity of the damage zones exhibit pronounced variations along the fault strike. We introduce the damage index as a proxy to quantify the extent of pre‐existing damage. We find a statistically significant anti‐correlation between the damage index and coseismic on‐fault slip. We thus infer that pre‐existing off‐fault damage plays a significant role in dissipating rupture energy, thereby reducing coseismic on‐fault slip. This study provides a natural case for linking the long‐term fault zone evolution and the short‐term earthquake rupture dynamics. Plain Language Summary: Large earthquakes can cause significant surface ruptures, which often spatially coincide with severe seismic disasters. Therefore, understanding where large coseismic slip occurs is crucial for mitigating hazards. Off‐fault damage is an indispensable component of fault zone structure, and its impact on seismic behavior has been widely emphasized. However, unlike coseismic off‐fault damage, pre‐existing off‐fault damage cannot be easily observed through remote sensing. Investigating pre‐existing off‐fault damage and its influence on coseismic on‐fault slip is challenging yet essential for comprehending earthquake processes. To address this gap, we conducted a detailed field investigation along the surface rupture of the 2008 Mw 7.9 Wenchuan earthquake, China, characterizing the along‐strike distribution of fault damage zone. Comparing the extent of pre‐existing fault damage with the coseismic on‐fault slip profiles revealed an inverse relationship: a higher extent of pre‐existing off‐fault damage leads to smaller coseismic on‐fault slip. We propose that the dissipation of seismic energy occurring within densely fractured damage zones provides a possible explanation for this phenomenon. Our findings establish critical connections between long‐term fault zone evolution and short‐term earthquake rupture dynamics. From a disaster reduction perspective, identifying off‐fault damage along major active faults before future earthquakes may enhance fault displacement hazard assessments. Key Points: Detailed measurements of the pre‐existing off‐fault damage along the surface ruptures associated with the 2008 Mw 7.9 Wenchuan EarthquakeWe provide compelling evidence that a higher extent of pre‐existing off‐fault damage leads to smaller coseismic on‐fault slipWe discuss the seismic energy dissipation hypothesis for the mechanism of pre‐existing off‐fault damage impeding coseismic on‐fault slip [ABSTRACT FROM AUTHOR]
- Published
- 2024
- Full Text
- View/download PDF