Poster #127, Fault and Rupture Mechanics (FARM)
Using Active Source Seismology to Image a Strike-Slip Fault Damage Zone as a Function of Depth, Distance, and Geology
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Poster Presentation
2021 SCEC Annual Meeting, Poster #127, SCEC Contribution #11130 VIEW PDF
r 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.
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