The break of earthquake asperities imaged by distributed acoustic sensing

Rupture imaging of megathrust earthquakes with global seismic arrays revealed frequency-dependent rupture signatures 1 – 4 , but the role of high-frequency radiators remains unclear 3 – 5 . Similar observations of the more abundant crustal earthquakes could provide critical constraints but are rare without ultradense local arrays 6 , 7 . Here we use distributed acoustic sensing technology 8 , 9 to image the high-frequency earthquake rupture radiators. By converting a 100-kilometre dark-fibre cable into a 10,000-channel seismic array, we image four high-frequency subevents for the 2021 Antelope Valley, California, moment-magnitude 6.0 earthquake. After comparing our results with long-period moment-release 10 , 11 and dynamic rupture simulations, we suggest that the imaged subevents are due to the breaking of fault asperities—stronger spots or pins on the fault—that substantially modulate the overall rupture behaviour. An otherwise fading rupture propagation could be promoted by the breaking of fault asperities in a cascading sequence. This study highlights how we can use the extensive pre-existing fibre networks 12 as high-frequency seismic antennas to systematically investigate the rupture process of regional moderate-sized earthquakes. Coupled with dynamic rupture modelling, it could improve our understanding of earthquake rupture dynamics.