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

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

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Digitization and Processing of J.M.A. Strong Motion Records 391and analysed <strong>the</strong> 17 seismograms (including 29 components which are all horizontal)<strong>from</strong> 9 great earthquakes around <strong>the</strong> Japan arcs recorded by <strong>the</strong> J.M.A. (orC.M.O.) low-magnification seismograph network. J.M.A. means <strong>the</strong> Japan MeteorologicalAgency and C.M.O. means <strong>the</strong> Central Meteorological Observatory. C.M.O.is <strong>the</strong> predecessor of J.M.A.In <strong>the</strong> following sections we describe in some detail <strong>the</strong> digitization and correctionprocedures of <strong>the</strong> records and <strong>the</strong>n compare <strong>the</strong> response spectra of <strong>the</strong> records with<strong>the</strong> Japanese seismic design specifications for large structures.2. RecordsTable 1 shows <strong>the</strong> list of <strong>the</strong> seismograms used in this analysis, and Figure 1shows <strong>the</strong> locations of <strong>the</strong> stations and <strong>the</strong> epicenters of <strong>the</strong> earthquakes. As shownin Table 1, <strong>the</strong>se earthquakes occurred <strong>from</strong> 1933 to 1983 and <strong>the</strong>ir magnitude, Ms,are between 7.6 and 8.5. The epicentral distances of <strong>the</strong> records axe between 49 and501 km.The type of seismograph which has been operating since about 1950 at <strong>the</strong> J.M.A.stations is <strong>the</strong> J.M.A. strong motion seismometer, and those which operated during<strong>the</strong> period <strong>from</strong> about 1930 to about 1950 at <strong>the</strong> C.M.O. stations are Omori’s,Imamura’s and C.M.O. strong motion seismographs. Hereafter we will call <strong>the</strong>latter <strong>the</strong> old type seismographs in this paper. Table 2 shows <strong>the</strong> characteristicsof each seismograph for each record. The range of <strong>the</strong> natural period of thoseseismographs is <strong>from</strong> 3.5 to 7.1 sec.Table 1. List of <strong>the</strong> <strong>Seismograms</strong>No. Date Earthquake Lat. Long. D Ms Station A ION OEEl 1933. 3. 3 Sanriku-Oki 39.25 144.50 - 8.5 Sendai 332 5E2 1938. 5.23 Iwaki-Oki 36.50 141.00 - 7.6 Mito 49 5E3 1938.11. 5 Fukushima-Ken- 36.75 141.75 60 7.7 Mito 122 5Toho-Oki( 1st .) Sendai 184 5E4 1938.11. 5 Fukushima-Ken- 37.25 141.75 60 7.7 Mto 150 4Toho-Oki(2nd.)E5 1938.11. 6 Fukushima-Ken- 37.25 142.25 60 7.6 Sendai 164 4Toho-0 ki( 3rd .) Mito 186 4E6 1944.12. 7 Tonankai 33.75 136.00 - 8.0 Murotomisaki 178 4Mishima 313 4E7 1946.12.21 Nankaido 32.50 134.50 - 8.2 Sumto 208 5Miyazaki 296 4E8 1968. 5.16 Tokachi-Oki 40.90 143.40 9 8.1 Akita 246 4Skata 377 3Niigat a 501 3E9 1983. 5.26 Nihonkai-Chubu 40.36 139.08 14 7.7 Mori 231 4Niigata 272 3Tomakomai 328 2No. = Earthquake number; Lat. = Epicenter latitude; Long. = Epicenter longitude;D = Depth in km; A = Epicentral Distance in km; I = Intensity (J.M.A. scale).

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