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

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1. IntroductionCatalogue of Chinese Earthquakes (M 2 6.5) 113Since <strong>the</strong> publication of a comprehensive catalogue of worldwide earthquakes byGutenberg and Richter (1954), Gutenberg (1956), Richter (1958), Duda (1965),RothC (1969), and o<strong>the</strong>rs have made supplements and revisions. As <strong>the</strong> instrumentcharacteristics, <strong>the</strong> magnitude scale and <strong>the</strong> measurement methods are different,<strong>the</strong>re is no unified standard for <strong>the</strong> magnitudes given in various catalogues, and evenfor different earthquakes in <strong>the</strong> same catalogue. Difficulties were encountered in <strong>the</strong>investigation of seismicity, earthquake prediction and hazard analysis based on suchdata, and incorrect conclusions were sometimes obtained. For example, using <strong>the</strong>catalogues given in Seismicity of <strong>the</strong> Earth and Associated Phenomena (Gutenbergand Richter, 1954) and Great Earthquakes 1896-1903 (Gutenberg, 1956), it was concludedthat <strong>from</strong> 1896 to 1906 <strong>the</strong> average annual energy release <strong>from</strong> earthquakesall over <strong>the</strong> world was about three times <strong>the</strong> average value for <strong>the</strong> years 1907 to1955. Through careful study, Kanamori and Abe (1979) pointed out that this wasdue to <strong>the</strong> underestimation of <strong>the</strong> effective magnification for <strong>the</strong> undamped Milneseismograph in <strong>the</strong> recording of great earthquakes. When proper corrections weremade (in some cases as large as 0.6 magnitude units), <strong>the</strong> abnormally high annualenergy release simply did not exist.Since <strong>the</strong> 1970s, seismologists began work on <strong>the</strong> unification of <strong>the</strong> earthquakemagnitude scale. In order to compile a catalogue of global earthquake activity witha uniform magnitude scale defined by Gutenberg and Richter (G-R scale), Gellerand Kanamori (1977), and Abe and Kanamori (1979) investigated in detail <strong>the</strong>magnitude scale used in Seismicity of <strong>the</strong> Earth and Associated Phenomena. Abeand Kanamori (1980) also studied <strong>the</strong> magnitudes of large shallow earthquakes <strong>from</strong>1953 to 1977. Abe (1981) recalculated <strong>the</strong> magnitudes of large shallow earthquakes<strong>from</strong> 1904 to 1980 with a uniform magnitude scale. Later, Abe and Noguchi (1983a)redetermined <strong>the</strong> magnitudes of large shallow shocks <strong>from</strong> 1898 to 1917 by correcting<strong>the</strong> magnification of undamped Milne and Omori seismographs. Thereafter,by re-evaluation of <strong>the</strong> quality of surface-wave magnitudes of shallow earthquakesbefore 1912, using <strong>the</strong> data given in <strong>the</strong> unpublished worksheets of Gutenberg andRichter (1954), Abe and Noguchi (198313) fur<strong>the</strong>r revised <strong>the</strong> average effective gainof <strong>the</strong> undamped Milne seismographs and redetermined <strong>the</strong> Ms of large shallowearthquakes in <strong>the</strong> period 1897 to 1912. Thus, a catalogue of worldwide large shallowearthquakes <strong>from</strong> 1897 to 1980 was completed with uniform magnitude scale.In 1971, <strong>the</strong> first edition of Catalogue of Chinese Earthquakes was published by<strong>the</strong> Central Seismological Group. Many editions were published successively, with<strong>the</strong> catalogues of <strong>the</strong> State Seismological Bureau (1977), Lee et al. (1978), and Gu(1983) used most often. In principle, all <strong>the</strong>se catalogues use <strong>the</strong> magnitudes given inGutenberg and Richter’s Seismicity of <strong>the</strong> Earth and Associated Phenomena or <strong>the</strong>irequivalents as standard (Gu, 1983). Actually, <strong>the</strong> data source is very complicated,<strong>the</strong> magnitude scale used is not <strong>the</strong> same, and detailed study and proper regressionanalysis were not carried out during <strong>the</strong> compilation. Therefore, <strong>the</strong> uniformity ofmagnitude in <strong>the</strong>se catalogues is not satisfactory.In compiling <strong>the</strong> fourth volume of <strong>the</strong> Compilation of <strong>Historical</strong> Materials of ChineseEarthquakes (Xie et al., 1985-86), we revised <strong>the</strong> parameters of all earthquakesthat occurred between 1900 and 1948 to prepare a catalogue with a uniform magnitudescale. In this paper, <strong>the</strong> magnitude scale used and <strong>the</strong> method of analysisare described, and <strong>the</strong> results of <strong>the</strong> revision are discussed.

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