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dc.contributor.author Wu Y.-M.
dc.contributor.author Chiao L.-Y.
dc.date.accessioned 2024-11-30T00:43:00Z
dc.date.available 2024-11-30T00:43:00Z
dc.date.issued 2006
dc.identifier https://www.elibrary.ru/item.asp?id=14283366
dc.identifier.citation Bulletin of the Seismological Society of America, 2006, 96, 1, 321-327
dc.identifier.issn 0037-1106
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/46686
dc.description.abstract The Chi-Chi, Taiwan, earthquake of 20 September 1999 was preceded by a notable decrease of the regional seismicity rate. The anomalous period started in January 1999 and lasted about 9 months, up to the occurrence of the mainshock, as revealed from analyzing the Taiwan catalog data from 1 January 1994 to 20 September 1999. Our results indicate that the mean seismicity rate is 435 events per month with a standard deviation of 78 events for earthquakes with magnitude above 2.0. During the anomalous period, seismicity rates fell outside the range of one standard deviation with a mean value of 314 events per month. There was also a consistent trend of decreasing regional b-value as well as notable increases of seismic activity in areas surrounding the Chi-Chi earthquake source region via the Z-test map (ZMAP) analysis.
dc.title SEISMIC QUIESCENCE BEFORE THE 1999 CHI-CHI, TAIWAN, MW 7.6 EARTHQUAKE
dc.type Статья
dc.identifier.doi 10.1785/0120050069


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