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| The first 20% of the full text of this article appears below. |
| INTRODUCTION |
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Let us first emphasize that a large number of seismic stations worldwide
recorded this event, and that many of these stations were not analyzed as part
of this study. For example, Ammon and Lay
(2007) demonstrate that a
number of stations in the North American USArray network, which is not part of
the IMS, have excellent recordings, some of them with a high signal-to-noise
ratio. Likewise, several IMS stations, e.g. in Russia and Mongolia,
detected the event but the recordings were not analyzed in this study. Our
main reason for not including these stations is that in a site-specific
capability study of the type discussed here, the resulting threshold is
dominated by a few stations of exceptionally high detection capability. We
have focused our analysis on these exceptional stations. In fact, as will be
shown later in this study, the monitoring capability of our selected network
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This article has been cited by other articles:
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P. G. Richards CTBT Monitoring: A Vital Activity for Our Profession Seismological Research Letters, May 1, 2008; 79(3): 375 - 378. [Full Text] [PDF] |
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