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Detecting Significant Stress Drop Variations in Large Micro-Earthquake Datasets: A Comparison Between a Convergent Step-Over in the San Andreas Fault and the Ventura Thrust Fault System, Southern California

Goebel, T. H. W. and Hauksson, E. and Plesch, A. and Shaw, J. H. (2017) Detecting Significant Stress Drop Variations in Large Micro-Earthquake Datasets: A Comparison Between a Convergent Step-Over in the San Andreas Fault and the Ventura Thrust Fault System, Southern California. Pure and Applied Geophysics, 174 (6). pp. 2311-2330. ISSN 0033-4553 . http://resolver.caltech.edu/CaltechAUTHORS:20170629-074538274

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Abstract

A key parameter in engineering seismology and earthquake physics is seismic stress drop, which describes the relative amount of high-frequency energy radiation at the source. To identify regions with potentially significant stress drop variations, we perform a comparative analysis of source parameters in the greater San Gorgonio Pass (SGP) and Ventura basin (VB) in southern California. The identification of physical stress drop variations is complicated by large data scatter as a result of attenuation, limited recording bandwidth and imprecise modeling assumptions. In light of the inherently high uncertainties in single stress drop measurements, we follow the strategy of stacking large numbers of source spectra thereby enhancing the resolution of our method. We analyze more than 6000 high-quality waveforms between 2000 and 2014, and compute seismic moments, corner frequencies and stress drops. Significant variations in stress drop estimates exist within the SGP area. Moreover, the SGP also exhibits systematically higher stress drops than VB and shows more scatter. We demonstrate that the higher scatter in SGP is not a generic artifact of our method but an expression of differences in underlying source processes. Our results suggest that higher differential stresses, which can be deduced from larger focal depth and more thrust faulting, may only be of secondary importance for stress drop variations. Instead, the general degree of stress field heterogeneity and strain localization may influence stress drops more strongly, so that more localized faulting and homogeneous stress fields favor lower stress drops. In addition, higher loading rates, for example, across the VB potentially result in stress drop reduction whereas slow loading rates on local fault segments within the SGP region result in anomalously high stress drop estimates. Our results show that crustal and fault properties systematically influence earthquake stress drops of small and large events and should be considered for seismic hazard assessment.


Item Type:Article
Related URLs:
URLURL TypeDescription
https://doi.org/10.1007/s00024-016-1326-8DOIArticle
https://link.springer.com/article/10.1007%2Fs00024-016-1326-8PublisherArticle
http://rdcu.be/tNqnPublisherFree ReadCube access
ORCID:
AuthorORCID
Hauksson, E.0000-0002-6834-5051
Additional Information:© 2016 Springer International Publishing. Received: 02 February 2016; Revised: 29 May 2016; Accepted: 30 May 2016; First Online: 13 June 2016. The initial manuscript benefitted from comments by Xiaowei Chen and Grzegorz Kwiatek. We would like to thank Michele Cooke for her detailed review. T. Goebel and E. Hauksson were supported by NEHRP/USGS grant G15AP00095 and the Southern California Earthquake Center (SCEC) under contribution number 12017 and 14033. SCEC is funded by NSF Cooperative Agreement EAR-0529922 and USGS Cooperative Agreement 07HQAG0008. We have used waveforms and parametric data from the Caltech/USGS Southern California Seismic Network (SCSN); DOI: 10.7914/SN/CI; stored at the Southern California Earthquake Center. DOI: 10.7909/C3WD3xH1.
Group:Seismological Laboratory
Funders:
Funding AgencyGrant Number
USGSG15AP00095
Southern California Earthquake Center (SCEC)UNSPECIFIED
NSFEAR-0529922
USGS07HQAG0008
Subject Keywords:Stress field heterogeneity; source parameter inversion; spatial stress drop variation; asperity strength; slip rates
Other Numbering System:
Other Numbering System NameOther Numbering System ID
Southern California Earthquake Center12017
Southern California Earthquake Center14033
Record Number:CaltechAUTHORS:20170629-074538274
Persistent URL:http://resolver.caltech.edu/CaltechAUTHORS:20170629-074538274
Official Citation:Goebel, T.H.W., Hauksson, E., Plesch, A. et al. Pure Appl. Geophys. (2017) 174: 2311. doi:10.1007/s00024-016-1326-8
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:78684
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:29 Jun 2017 15:08
Last Modified:29 Jun 2017 15:08

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