Exciting news! We're transitioning to the Statewide California Earthquake Center. Our new website is under construction, but we'll continue using this website for SCEC business in the meantime. We're also archiving the Southern Center site to preserve its rich history. A new and improved platform is coming soon!

Using Active Source Seismology to Image a Strike-Slip Fault Damage Zone as a Function of Depth, Distance, and Geology

Travis V. Alongi, Emily E. Brodsky, Jared W. Kluesner, & Daniel S. Brothers

Published August 2, 2021, SCEC Contribution #11130, 2021 SCEC Annual Meeting Poster #127 (PDF)

Poster Image: 
Fault damage zones provide a window into the non-elastic processes and products of an earthquake, but geological and seismic tomography methods have limited resolution and in particular have been unable to measure damage zones at depth with sufficient resolution to separately resolve depth, distance and lithological variations. Here, we identify and analyze the damage zone of the Palos Verdes Fault in offshore southern California using two existing 3D seismic reflection datasets. We use a novel algorithm applied to the seismic data to identify seismic discontinuities attributed to faults and fractures in large seismic volumes (~ 10^8 points) and examine the spatial distribution of damage. Our results from the Palo Verdes Fault zone show that damage is focused around mapped faults and that damage decays with distance from the mapped fault, reaching a clearly defined relatively undamaged background region at a distance of 2.5 km from the fault. The damaged zone obeys power law-like behavior at the outer edges of a 3-strand fault network, with a power law exponent of ~0.7, and this trend may be extrapolated to a probability of 1 at the mapped main (central) fault strand location. The power law like dependence of the damage zone with distance from fault is like outcrop studies. However, here we extend the study to distances seldom accessible. We find that fracturing in the damage zone increases with depth to around 500 m and at greater depths damage may be more strongly controlled by lithologiy, induration, and unit thickness than depth variations.

Key Words
Fault damage zone, Fault scaling, Fault zone complexity, Marine active source seismology, Fault zone imaging, Borderlands, Palos Verdes Fault

Citation
Alongi, T. V., Brodsky, E. E., Kluesner, J. W., & Brothers, D. S. (2021, 08). Using Active Source Seismology to Image a Strike-Slip Fault Damage Zone as a Function of Depth, Distance, and Geology. Poster Presentation at 2021 SCEC Annual Meeting.


Related Projects & Working Groups
Fault and Rupture Mechanics (FARM)