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Historical Seismograms - Evidence from the AD 2000 Izu Islands ...

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D. M. McGregor, A. A. Hughes, and R. D. AdamsDuring analysis, <strong>the</strong> computer program first groups toge<strong>the</strong>r origin estimatesof <strong>the</strong> same earthquake <strong>from</strong> different agencies, and <strong>the</strong>n associates <strong>the</strong> individualstation readings with <strong>the</strong> most likely event. In a typical month up to 100,000 stationreadings are analysed, and initially between 1,600 and 2,000 events are identified.After mis-associations have been remedied and o<strong>the</strong>r discrepancies rectified, <strong>the</strong>remaining unassociated readings are searched for new events, and usually about250 previously unlocated earthquakes are added to <strong>the</strong> file. Thus, <strong>the</strong> number ofevents listed each month is usually between 1,800 and 2,300. The delay of two yearsin <strong>the</strong> publication of <strong>the</strong> final bulletin is justified by <strong>the</strong> fact that this number ofevents is several times greater than that obtained by <strong>the</strong> Prelimin,wy Determinationof Epicenters Service of <strong>the</strong> U. S. Geological Survey, whose aim is to produce a rapidservice for well-reported larger events, compared with ISC’s wish for completeness,at <strong>the</strong> expense of speed.3. Publications3.1. Bulletin of <strong>the</strong> International Seismological CentreThe Bulletin is <strong>the</strong> Centre’s main publication, containing all relevant informationfor a given month’s earthquakes. For each event, <strong>the</strong> origin estimates given byo<strong>the</strong>r agencies are listed, followed by <strong>the</strong> refined estimate calculated by <strong>the</strong> Centre.This gives origin time, latitude, longitude and depth with computer determinedstandard errors. The earthquake’s felt effects and any unusual scientific featuresare also described. Magnitudes mb and Ms are calculated when individual stationsreport readings of amplitude and period, or <strong>the</strong>ir ratio. Since <strong>the</strong> data-yeax 1978 aneffort has been made to obtain more long-period readings, and consequently moredeterminations of Ms.For some small earthquakes located by national agencies <strong>the</strong> origin co-ordinatesonly can be given, but for better observed earthquakes observations <strong>from</strong> individualseismograph stations are listed with <strong>the</strong>ir distance, azimuth and time residual. For<strong>the</strong> largest earthquakes <strong>the</strong> number of reporting stations can reach more than 600.The Bulletin provides seismologists with <strong>the</strong> fullest available information on allaspects of observational seismology necessary for <strong>the</strong> study of earthquake occurrenceand earth structure. All issues of <strong>the</strong> Bulletin since 1964 are in fixed field formatavailable on magnetic tape.3.2. Regional Catalogue of EarthquakesThis is a six-monthly compilation of earthquake origin parameters and felt information,without <strong>the</strong> detailed station observations of <strong>the</strong> Bulletin. It containslists of ‘major earthquakes” above certain magnitudes, reports of “felt and damagingearthquakes”, “probable explosions”, and <strong>the</strong> main regional catalogue in whichall events in given geographic regions are listed toge<strong>the</strong>r. This publication is thatmost relevant to detailed studies of seismicity, and <strong>the</strong> one most sought by institutionssuch as consulting engineering firms and insurance companies. It is publishedshortly after <strong>the</strong> issues of <strong>the</strong> Bulletin for June and December of each year. Like <strong>the</strong>Bulletin recent issues of <strong>the</strong> Catalogue are available in fixed field format on magnetictape. It also gives world-wide lists of seismograph stations and <strong>the</strong>ir coordinates.

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