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Title: Precise Relative Earthquake Magnitudes from Cross Correlation

Abstract

We present a method to estimate precise relative magnitudes using cross correlation of seismic waveforms. Our method incorporates the intercorrelation of all events in a group of earthquakes, as opposed to individual event pairings relative to a reference event. This method works well when a reliable reference event does not exist. We illustrate the method using vertical strike-slip earthquakes located in the northeast Pacific and Panama fracture zone regions. Our results are generally consistent with the Global Centroid Moment Tensor catalog, which we use to establish a baseline for the relative event sizes.

Authors:
 [1];  [2]
  1. Los Alamos National Lab. (LANL), Los Alamos, NM (United States)
  2. Pennsylvania State Univ., State College, PA (United States)
Publication Date:
Research Org.:
Los Alamos National Lab. (LANL), Los Alamos, NM (United States)
Sponsoring Org.:
USDOE
OSTI Identifier:
1239272
Report Number(s):
LA-UR-14-28088
Journal ID: ISSN 0037-1106
Grant/Contract Number:  
AC52-06NA25396
Resource Type:
Accepted Manuscript
Journal Name:
Bulletin of the Seismological Society of America
Additional Journal Information:
Journal Volume: 105; Journal Issue: 3; Journal ID: ISSN 0037-1106
Publisher:
Seismological Society of America
Country of Publication:
United States
Language:
English
Subject:
58 GEOSCIENCES

Citation Formats

Cleveland, K. Michael, and Ammon, Charles J. Precise Relative Earthquake Magnitudes from Cross Correlation. United States: N. p., 2015. Web. doi:10.1785/0120140329.
Cleveland, K. Michael, & Ammon, Charles J. Precise Relative Earthquake Magnitudes from Cross Correlation. United States. https://doi.org/10.1785/0120140329
Cleveland, K. Michael, and Ammon, Charles J. Tue . "Precise Relative Earthquake Magnitudes from Cross Correlation". United States. https://doi.org/10.1785/0120140329. https://www.osti.gov/servlets/purl/1239272.
@article{osti_1239272,
title = {Precise Relative Earthquake Magnitudes from Cross Correlation},
author = {Cleveland, K. Michael and Ammon, Charles J.},
abstractNote = {We present a method to estimate precise relative magnitudes using cross correlation of seismic waveforms. Our method incorporates the intercorrelation of all events in a group of earthquakes, as opposed to individual event pairings relative to a reference event. This method works well when a reliable reference event does not exist. We illustrate the method using vertical strike-slip earthquakes located in the northeast Pacific and Panama fracture zone regions. Our results are generally consistent with the Global Centroid Moment Tensor catalog, which we use to establish a baseline for the relative event sizes.},
doi = {10.1785/0120140329},
journal = {Bulletin of the Seismological Society of America},
number = 3,
volume = 105,
place = {United States},
year = {Tue Apr 21 00:00:00 EDT 2015},
month = {Tue Apr 21 00:00:00 EDT 2015}
}

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Cited by: 13 works
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Works referencing / citing this record:

Real-time envelope cross-correlation detector: application to induced seismicity in the Insheim and Landau deep geothermal reservoirs
journal, August 2016