Coronavirus Information for the UC San Diego Community

Our leaders are working closely with federal and state officials to ensure your ongoing safety at the university. Stay up to date with the latest developments. Learn more.

Basic data features and results from a spatially dense seismic array on the San Jacinto fault zone

TitleBasic data features and results from a spatially dense seismic array on the San Jacinto fault zone
Publication TypeJournal Article
Year of Publication2015
AuthorsBen-Zion Y., Vernon FL, Ozakin Y., Zigone D., Ross Z.E, Meng H.R, White M., Reyes J., Hollis D., Barklage M.
JournalGeophysical Journal International
Date Published2015/07
Type of ArticleArticle
ISBN Number0956-540X
Accession NumberWOS:000360623400024
Keywordsdouble-difference tomography; earthquake; field; ground motion; Guided waves; noise; radiation; Seismic attenuation; seismic tomography; Site effects; site response; southern california; temporal-changes; velocity changes; wave propagation; Wave scattering and diffraction

We discuss several outstanding aspects of seismograms recorded during >4 weeks by a spatially dense Nodal array, straddling the damage zone of the San Jacinto fault in southern California, and some example results. The waveforms contain numerous spikes and bursts of high-frequency waves (up to the recorded 200 Hz) produced in part by minute failure events in the shallow crust. The high spatial density of the array facilitates the detection of 120 small local earthquakes in a single day, most of which not detected by the surrounding ANZA and regional southern California networks. Beamforming results identify likely ongoing cultural noise sources dominant in the frequency range 1-10 Hz and likely ongoing earthquake sources dominant in the frequency range 20-40 Hz. Matched-field processing and back-projection of seismograms provide alternate event location. The median noise levels during the experiment at different stations, waves generated by Betsy gunshots, and wavefields from nearby earthquakes point consistently to several structural units across the fault. Seismic trapping structure and local sedimentary basin produce localized motion amplification and stronger attenuation than adjacent regions. Cross correlations of high-frequency noise recorded at closely spaced stations provide a structural image of the subsurface material across the fault zone. The high spatial density and broad frequency range of the data can be used for additional high resolution studies of structure and source properties in the shallow crust.

Student Publication: