| Strong earthquake activity all over the world and strong-moderate earthquake activity within and near China (August, 2000 ~ September, 2000) |
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| 作者姓名： | 陈培善 |
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| 作者单位： | Institute of Geophysics, China Seismological Bureau,
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| 摘 要： | IllustrationAll the data in this catalog are chosen from the (Preliminary Seismological Report of Chinese Seismic Stations( (Its abbreviation is (Monthly Report(). The catalog includes the events of M(4.7 in and near China and M(6 all over the world. The (Monthly Report( is monthly compiled by the Ninth Section of Institute of Geophysics, CSB.The origin times of earthquakes in the catalog adopt coordinated universal time (UTC) in accordance with international convention. The location…
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Strong earthquake activity all over the world and strong-moderate earthquake activity within and near China (August, 2000 ~ September, 2000) |
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| CHEN Pei-shan.Strong earthquake activity all over the world and strong-moderate earthquake activity within and near China (August, 2000 ~ September, 2000)[J].Acta Seismologica Sinica(English Edition),2001,14(1). |
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| Authors: | CHEN Pei-shan |
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| Abstract: | Illustration All the data in this catalog are chosen from the 2Preliminary Seismological Report of Chine-se Seismic Stations2 (Its abbreviation is 2Monthly Report2). The catalog includes the events of M34.7 in and near China and M36 all over the world. The 2Monthly Report2 is monthly compiled by the Ninth Section of Institute of Geophysics, CSB. The origin times of earthquakes in the catalog adopt coordinated universal time (UTC) in accordance with international convention. The location of every epicenter is expressed by its latitude and longitude, at the same time by the corresponding geographical region proposed by Flinn and Engdahl. The regional names are only for references and do not imply any political significance. The number of stations used and standard deviation are also given in order to illus-trate the precision of location. The surface wave magnitude MS is measured from the records of intermediate period broad band SK seismographs and adopting the surface wave magnitude formula of Beijing Station of 1965: MS= lg(AH/T)+1.66lgD +3.5 (1°
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