SCEC2024 Poster #010: Aftershock interferometry illuminates the fault zone beneath the Noto peninsula

Group B, Poster #010, Seismology

Aftershock interferometry illuminates the fault zone beneath the Noto peninsula

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Poster Presentation

2024 SCEC Annual Meeting, Poster #010, SCEC Contribution #13546 VIEW PDF

Using interferometry, aftershocks of large earthquakes can be treated as a network of virtual seismometers to allow detailed imagery along the fault trace. The Virtual Seismometer Method (VSM) is a technique that provides precise estimates of the Green Function (GF) between earthquakes (Curtis et al., 2009; Hong and Menke, 2006). In simple terms, VSM involves correlating the record of a pair of events recorded at an individual station and then stacking the results over all stations to obtain the final correlation waveform. By effectively replacing each earthquake with a "virtual seismometer" recording all the others, the technique isolates the portion of the data that is sensitive ...to the source region and dramatically increases our ability to see into tectonically active features where seismic stations either can't or haven't been located, such as at depth in active fault zones.

On January 1st, 2024, a large (Mw 7.5) earthquake occurred beneath the Noto Peninsula in Japan, causing extensive damage and affecting tens of thousands of people. This triggered an aftershock sequence with thousands of smaller events extending across the entire peninsula and into the Sea of Japan. On January 3rd, we identified records for dozens of high quality events recorded by the dense Japanese seismic network at sensors 100-300 km away. Green functions were calculated for hundreds of paths, illuminating a section of the fault zone roughly 90 km long and 10 km wide. We inverted the resulting waveforms to create a localized image of the seismic velocity and attenuation structure throughout the crust with kilometer scale lateral resolution.

At the higher resolution, the northeast trending fault trace resolves into a series of sub-parallel fractures. The ratios of seismic attenuation (Qp/Qs) help to identify separate tectonic regimes. In particular the seismogenic zone, defined by the full catalog of events, falls within the contours of higher Qp/Qs which has a topographically complex interface with a deeper, distinctly lower Qp/Qs region. The main event initiated directly above the feature with the lowest Qp/Qs value.

Data were obtained via the National Research Institute for Earth Science and Disaster Resilience (2019), NIED Hi-net, National Research Institute for Earth Science and Disaster Resilience, doi:10.17598/NIED.0003

This work performed under the auspices of the U.S. Department of Energy by Lawrence Livermore National Laboratory under Contract DE-AC52-07NA27344.
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