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Max Wyss
Reporting history of the Central Aleutians Seismograph Network and the quiescence preceding the 1986 Andreanof Island earthquake
Bulletin of the Seismological Society of America (August 1991), 81(4):1231-1254
Abstract: Index Terms/Descriptors: Latitude & Longitude:
GeoRef, Copyright 2004, American Geological Institute.
The earthquake catalog of the Central Aleutian Seismic Network (CASN) was searched systematically for significant rate changes in the period from 1976 through 1985. The magnitude signatures for the nine changes were modeled by synthetic signatures. By this method, six of the rate changes could be identified as artificial, based on the criteria that the rate change was confined to small magnitude events and that magnitude shifts were present. For each of these changes an artificial cause existed that affected the network within one to two months of the time of change as estimated from the catalog analysis. One of these cases was a rate decrease by a factor of 2 associated with a storm that had put out of operation two thirds of the network. Another change coincided with the introduction of digital data processing. The four remaining cases were artificial reporting rate increases due to instaliation of several new stations or to repair of several stations that had failed. The three rate changes that could not be identified unambiguously as artificial or natural on the basis of magnitude signatures were all rate decreases by factors of approximately 2. Two of these were clearly due to disasters that had put out of operation more than half of the network. The third was the proposed precursory quiescence to the 1986 Andreanof island (M = 7.9) earthquake. From this we conclude that, without knowledge of the network history, many of the artificial reporting rate changes in earthquake catalogs can be identified as artificial and that their onset time can be estimated to within one to two months. An earthquake count, independent from the Adak catalog, was obtained from the Helicorder records of the station Adak for the years 1978 through 1985 for the vicinity of Adak island. Of a total of 1831 events, 335 were not in the Adak catalog and 981 were located within the 1986 aftershock area. The Helicorder earthquake count showed a pronounced decrease by about 50 per cent, similar in amount to that in the Adak catalog.
Alaska; Andreanof Islands earthquake 1986; arrays; catalogs; Central Aleutians Seismograph Network; earthquakes; magnitude; networks; precursors; seismic quiescence; seismicity; seismograms; seismology; southwestern Alaska; United States
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