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How to Invert Multi-Band, Regional Phase Amplitudes for 2-D Attenuation and Source Parameters: Tests Using the USArray

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Abstract

We inverted for laterally varying attenuation, absolute site terms, moments and apparent stress using over 460,000 Lg amplitudes recorded by the USArray for frequencies between 0.5 and 16 Hz. Corner frequencies of Wells, Nevada, aftershocks, obtained by independent analysis of coda spectral ratios, controlled the tradeoff between attenuation and stress, while independently determined moments from St. Louis University and the University of California constrained absolute levels. The quality factor, Q, was low for coastal regions and interior volcanic and tectonic areas, and high for stable regions such as the Great Plains, and Colorado and Columbia Plateaus. Q increased with frequency, and the rate of increase correlated inversely with 1-Hz Q, with highest rates in low-Q tectonic regions, and lowest rates in high-Q stable areas. Moments matched independently determined moments with a scatter of 0.2 NM. Apparent stress ranged from below 0.01 to above 1 MPa, with means of 0.1 MPa for smaller events, and 0.3 MPa for larger events. Stress was observed to be spatially coherent in some areas; for example, stress was lower along the San Andreas fault through central and northern California, and higher in the Walker Lane, and for isolated sequences such as Wells. Variance reduction relative to 1-D models ranged from 50 to 90 % depending on band and inversion method. Parameterizing frequency dependent Q as a power law produced little misfit relative to a collection of independent, multi-band Q models, and performed better than the omega-square source parameterization in that sense. Amplitude residuals showed modest, but regionally coherent patterns that varied from event to event, even between those with similar source mechanisms, indicating a combination of focal mechanism, and near source propagation effects played a role. An exception was the Wells mainshock, which produced dramatic amplitude patterns due to its directivity, and was thus excluded from the inversions. The 2-D Q plus absolute site models can be used for high accuracy, broad area source spectra, magnitude and yield estimation, and, in combination with models for all regional phases, can be used to improve discrimination, in particular for intermediate bands that allow coverage to be extended beyond that available for high frequency P-to-S discriminants.

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Acknowledgments

This study relied on waveform and ancillary data collected by the Earthscope USArray project. Waveforms we used included contributions from the ANZA Regional, Berkeley Digital Seismograph, Caltech Regional Seismic, Global Seismograph, Western Great Basin, USArray Transportable, US National Seismic, and U. Utah Regional networks. We further acknowledge the Array Operations Facility (NMT), the Array Network Facility (UCSD), and the IRIS Data Mangement Center for efforts to collect and archive USArray data for use by the scientific community. We also thank Robert Herrmann, Douglas Dreger, and students for their timely production of moment tensor results for public consumption. SAC and GMT software were used for processing and display. We greatly appreciate input from two anonymous reviewers. WSP thanks Mark Fisk for discussions about application of source constraints in Asia, and Michael Fehler for introducing the author to source parameter-attenuation inversions many years ago. Publication of this research was supported by the US DOE under contract DE-AC52-06NA25396.

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  1. Los Alamos National Laboratory, Los Alamos, USA

    W. Scott Phillips

  2. Weston Geophysical, Lexington, USA

    Kevin M. Mayeda

  3. Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy

    Luca Malagnini

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  1. W. Scott Phillips
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Correspondence to W. Scott Phillips.

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Phillips, W.S., Mayeda, K.M. & Malagnini, L. How to Invert Multi-Band, Regional Phase Amplitudes for 2-D Attenuation and Source Parameters: Tests Using the USArray. Pure Appl. Geophys. 171, 469–484 (2014). https://doi.org/10.1007/s00024-013-0646-1

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