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dc.contributor.authorShare, Pieter-Ewald
dc.contributor.authorAllam, Amir A.
dc.contributor.authorBen-Zion, Yehuda
dc.contributor.authorLin, Fan-Chi
dc.contributor.authorVernon, Frank L.
dc.date.accessioned2021-03-09T10:53:09Z
dc.date.available2021-03-09T10:53:09Z
dc.date.issued2018-09-18
dc.date.submitted2018-05-27
dc.identifier.citationShare, P.-E., Allam, A. A., Ben-Zion, Y., Lin, F.-C., & Vernon, F. L. (2018). Structural Properties of the San Jacinto Fault Zone at Blackburn Saddle from Seismic Data of a Dense Linear Array. Pure and Applied Geophysics, 176(3), 1169–1191. doi:10.1007/s00024-018-1988-5
dc.identifier.issn0033-4553
dc.identifier.issn1420-9136
dc.identifier.doi10.1007/s00024-018-1988-5
dc.identifier.urihttp://hdl.handle.net/10754/667991
dc.description.abstractWe image the San Jacinto fault zone at Blackburn Saddle using earthquake waveforms recorded by a ~ 2-km across-fault linear array with 108 three-component sensors separated by ~ 10–30 m. The length and spatiotemporal sampling of the array allow us to derive high-resolution information on the internal fault zone structure with spatial extent that can be merged with regional tomography models. Across-fault variations in polarization, amplitude, and arrival time of teleseismic P waves indicate abrupt changes in subsurface structure near the surface trace of the fault (sensor BS55) and ~ 270 m to the northeast (sensor BS34). Analysis of fault zone head waves from local events reveals the existence of a deep bimaterial interface that extends from the array to at least 50 km southeast and has a section with > 10% velocity contrast. This analysis also corroborates the teleseismic results and indicates a broad damage zone primarily northeast of the fault bounded by a shallow bimaterial interface near BS34 that merges with the deep interface. Detection and waveform inversions of Love-type fault zone trapped waves generated by local events indicate a trapping structure within the broader damage zone with width of ~ 150 m, velocity reduction of ~ 55% from the surrounding rock and depth extent of ~ 2 km. The performed analyses provide consistent results on the subsurface location of the main seismogenic fault and properties of a major bimaterial interface and damage structure. The imaged fault zone properties are consistent with preferred propagation direction of earthquake ruptures in the area to the northwest.
dc.description.sponsorshipWe thank Marianne Karplus and Jerry Schuster for providing geophones for the experiment, and Hsin-Hua Huang, Elizabeth Berg, Yadong Wang, Scott Palmer, Kathleen Ritterbush, Jon Gonzalez, Jerry Schuster, Robert Zinke and Cooper W. Harris for assistance during the array deployment. The research was supported by the King Abdullah University of Science and Technology (Award OCRF-2014-CRG3-2300), the National Science Foundation (Grants CyberSEES-1442665 and EAR-1620601), and the Department of Energy (Awards DESC0016520 and DE-SC0016527). The data collected with the BS array are stored at the University of Utah Seismograph Stations and are available upon request. Most maps are made using the Generic Mapping Tools (Wessel et al. 2013). The manuscript benefitted from useful comments by two anonymous referees.
dc.publisherSpringer Nature
dc.relation.urlhttp://link.springer.com/10.1007/s00024-018-1988-5
dc.rightsArchived with thanks to Pure and Applied Geophysics
dc.titleStructural Properties of the San Jacinto Fault Zone at Blackburn Saddle from Seismic Data of a Dense Linear Array
dc.typeArticle
dc.identifier.journalPure and Applied Geophysics
dc.eprint.versionPost-print
dc.contributor.institutionDepartment of Earth Sciences, University of Southern California, Los Angeles, CA, 90089, United States
dc.contributor.institutionDepartment of Geology and Geophysics, The University of Utah, Salt Lake City, UT, 84112, United States
dc.contributor.institutionScripps Institution of Oceanography, University of California San Diego, La Jolla, CA, 92093, United States
dc.identifier.volume176
dc.identifier.issue3
dc.identifier.pages1169-1191
kaust.grant.numberOCRF-2014-CRG3-2300
dc.date.accepted2018-09-03
dc.identifier.eid2-s2.0-85056179298


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