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Title: Pickless event detection and location: The waveform correlation event detection system (WCEDS) revisited

The standard paradigm for seismic event monitoring breaks the event detection problem down into a series of processing stages that can be categorized at the highest level into station-level processing and network-level processing algorithms (e.g., Le Bras and Wuster (2002)). At the station-level, waveforms are typically processed to detect signals and identify phases, which may subsequently be updated based on network processing. At the network-level, phase picks are associated to form events, which are subsequently located. Furthermore, waveforms are typically directly exploited only at the station-level, while network-level operations rely on earth models to associate and locate the events that generated the phase picks.
Authors:
 [1] ;  [1] ;  [1] ;  [1]
  1. Sandia National Laboratories (SNL-NM), Albuquerque, NM (United States)
Publication Date:
Report Number(s):
SAND-2016-0074J
Journal ID: ISSN 0037-1106; 617561
Grant/Contract Number:
AC04-94AL85000
Type:
Accepted Manuscript
Journal Name:
Bulletin of the Seismological Society of America
Additional Journal Information:
Journal Name: Bulletin of the Seismological Society of America; Journal ID: ISSN 0037-1106
Publisher:
Seismological Society of America
Research Org:
Sandia National Lab. (SNL-NM), Albuquerque, NM (United States)
Sponsoring Org:
USDOE National Nuclear Security Administration (NNSA), Office of Defense Nuclear Nonproliferation (NA-20)
Country of Publication:
United States
Language:
English
Subject:
58 GEOSCIENCES
OSTI Identifier:
1246336

Arrowsmith, Stephen John, Young, Christopher J., Ballard, Sanford, and Slinkard, Megan Elizabeth. Pickless event detection and location: The waveform correlation event detection system (WCEDS) revisited. United States: N. p., Web. doi:10.1785/0120160018.
Arrowsmith, Stephen John, Young, Christopher J., Ballard, Sanford, & Slinkard, Megan Elizabeth. Pickless event detection and location: The waveform correlation event detection system (WCEDS) revisited. United States. doi:10.1785/0120160018.
Arrowsmith, Stephen John, Young, Christopher J., Ballard, Sanford, and Slinkard, Megan Elizabeth. 2016. "Pickless event detection and location: The waveform correlation event detection system (WCEDS) revisited". United States. doi:10.1785/0120160018. https://www.osti.gov/servlets/purl/1246336.
@article{osti_1246336,
title = {Pickless event detection and location: The waveform correlation event detection system (WCEDS) revisited},
author = {Arrowsmith, Stephen John and Young, Christopher J. and Ballard, Sanford and Slinkard, Megan Elizabeth},
abstractNote = {The standard paradigm for seismic event monitoring breaks the event detection problem down into a series of processing stages that can be categorized at the highest level into station-level processing and network-level processing algorithms (e.g., Le Bras and Wuster (2002)). At the station-level, waveforms are typically processed to detect signals and identify phases, which may subsequently be updated based on network processing. At the network-level, phase picks are associated to form events, which are subsequently located. Furthermore, waveforms are typically directly exploited only at the station-level, while network-level operations rely on earth models to associate and locate the events that generated the phase picks.},
doi = {10.1785/0120160018},
journal = {Bulletin of the Seismological Society of America},
number = ,
volume = ,
place = {United States},
year = {2016},
month = {1}
}