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Detection of the Wenchuan aftershock sequence using waveform correlation with a composite regional network

Bulletin of the Seismological Society of America

Slinkard, Megan E.; Heck, Stephen L.; Bonal, Nedra; Daily, David M.; Young, Christopher J.

Using template waveforms from aftershocks of the Wenchuan earthquake (12 May 2008, Ms 7.9) listed in a global bulletin and continuous data from eight regional stations, we detected more than 6000 additional events in the mainshock source region from 1 May to 12 August 2008. These new detections obey Omori’s law, extend the magnitude of completeness downward by 1.1 magnitude units, and lead to a more than fivefold increase in number of known aftershocks compared with the global bulletins published by the International Data Centre and the International Seismological Centre. Moreover, we detected more M >2 events than were listed by the Sichuan Seismograph Network. Several clusters of these detections were then relocated using the double-difference method, yielding locations that reduced travel-time residuals by a factor of 32 compared with the initial bulletin locations. Our results suggest that using waveform correlation on a few regional stations can find aftershock events very effectively and locate them with precision.

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GeoTess: A generalized Earth model software utility

Seismological Research Letters

Ballard, Sanford; Hipp, James R.; Kraus, Brian; Encarnacao, Andre V.; Young, Christopher J.

GeoTess is a model parameterization and software support library that manages the construction, population, storage, and interrogation of data stored in 2D and 3D Earth models. The software is available in Java and C++, with a C interface to the C++ library. The software has been tested on Linux, Mac, Sun, and PC platforms. It is open source and is available online (see Data and Resources).

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

Bulletin of the Seismological Society of America

Arrowsmith, Stephen J.; Young, Christopher J.; Ballard, Sanford; Slinkard, Megan E.

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.

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Results 126–150 of 271
Results 126–150 of 271