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

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324 S. Riad, H. Meyers, and C. KisslingerTable 1. Flinn-Engdahl Seismic Regions Included in the Middle East CatalogNo. Geographical Region No. Geographical Region34 13423433443453463473483493503513523533543553563663673693713723 73374375Iran-USSR Border Region 401Turkmen-Afghanistan Border Region 415Turkey-Iran Border Region 416N.W. Iran-USSR Border Region 417Northwestern Iran 418Iran-Iraq Border Region 419Western Iran 552Iran 553Northwestern Afghanistan 554Southwestern Afghanistan 555Eastern Arabian Peninsula 556Persian Gulf 557Southern Iran 558Western Pakistan 559Gulf of Oman 560Near Coast of West Pakistan 571Turkey 709Turkey-USSR Border Region 710Dodecanese Islands 711Eastern Mediterranean Sea 712CypruB 717Dead Sea Region 718Jordan-Syria Region 720IraqNear Coast of LibyaEastern Gulf of AdenSocotra RegionArabian SeaLaccadive Islands RegionNortheastern SomaliaLibyaUnited Arab RepublicRed SeaWestern Arabian PeninsulaCentral AfricaSudanEthiopiaWestern Gulf of AdenNorthwestern SomaliaSouthern SomaliaAfghanistanPakist anSouthwestern KashmirIndia-Pakistan Border RegionAfghanistan-USSR Border RegionHindu Kush RegionNorthwestern KashmirRouhban, 1983). The total number of earthquakes collected in the first stage wasmore than 22,000. This number was reduced to about 8,000 by limiting the investigationto events of magnitude 2 4.5 or of intensity I, 2 VI. Of these 8,000events, 2,400 were reported as suspected duplicates, and were removed by reviewingthe different sources of data. Preference was given to sources that reevaluatedearthquake parameters and to those including more complete or recent information.After removing the duplicates, reported values of the different parameters for thesame event (e.g., mb, Ms, Mr,, and I,) were used to obtain relations between theseparameters. Magnitudes given without indications of their type were grouped undercatagory M,. They were found to be approximately equal to Ms, but werenot identical. The relations thus obtained were used to assign missing values ofall parameters to the events included in the catalog. According to the obtainedrelations a lower limit of Ms 2 3.9, which is approximately equal to mg 2 4.5 andI, 2 V, was considered for the catalog and the accompanying seismicity map forthe Middle East. A summary of the earthquakes included in the catalog is given inTable 2.2. Magnitude-Magnitude RelationsNormally, magnitudes based on surface and body waves are different for the sameearthquake. This is because mb and Ms sample different parts of the characteristicearthquake spectrum. It has been noted by Gutenberg and Richter (1954) that thedifference between mb and M, is a function of magnitude, and so it follows thatthe magnitude scales based on surface and body waves are not consistent with eachother.
On the Seismicity of the Middle East 325Table 2. Summary of the Middle East Catalog by Year and Magnitude MsYear Mag Less 3.9 4.5 5.0 5.5 6.0 6.5 7.0 7.5 8.0 8.5 Totalsnot than to to to to to to to to to togiven 3.9 4.4 4.9 5.4 5.9 6.4 6.9 7.4 7.9 8.4 8.91900 0 0 0 0 2 1 0 0 0 0 0 0 31901 0 0 4 3 2 1 0 0 0 0 0 0 101902 0 0 1 3 2 0 0 2 0 0 0 0 81903 0 0 0 2 8 4 2 2 0 0 0 0 181904 0 0 3 5 1 7 3 0 0 0 0 0 191905 0 0 1 6 5 3 1 2 1 0 0 0 191906 0 0 2 1 2 2 1 2 0 0 0 0 101907 0 0 5 4 4 0 3 1 1 0 0 0 181908 0 0 0 8 6 2 1 2 1 0 0 0 201909 1 0 0 2 5 3 0 2 2 1 0 0 161910 0 0 1 4 3 1 2 0 0 0 0 0 111911 1 0 0 0 1 1 2 2 1 1 0 0 91912 0 0 1 4 2 3 3 3 0 1 0 0 171913 1 0 0 2 6 1 1 0 0 0 0 0 111914 0 0 9 10 2 0 0 3 2 0 0 0 261915 0 0 2 0 5 1 1 1 0 0 0 0 101916 0 0 4 4 0 0 1 0 1 0 0 0 101917 0 0 2 5 2 3 0 0 1 0 0 0 131918 0 0 0 5 7 5 1 0 0 0 0 0 181919 0 0 6 8 1 0 4 0 0 1 0 0 0 291920 0 0 2 6 7 3 0 0 0 0 0 0 181921 0 0 0 3 8 3 0 1 0 0 1 0 161922 0 0 0 6 4 1 2 1 0 1 0 0 151923 0 0 2 4 6 2 1 3 0 0 0 0 181924 0 0 4 13 8 4 3 1 1 0 0 0 341925 0 0 13 2014 9 1 0 0 0 0 0 571926 0 0 4 1 9 1 7 1 0 0 1 0 1 2 0 541927 0 0 4 4 5 2 6 0 0 0 0 0 211928 0 0 10 1010 4 5 2 0 0 0 0 411929 0 0 9 14 10 8 4 0 2 0 0 0 471930 0 0 1 0 2 1 1 6 4 0 0 0 1 0 0 521931 0 0 7 12 12 3 4 2 2 0 0 0 421932 0 0 10 7 1 8 2 0 0 0 0 0 0 371933 0 0 3 8 9 3 2 1 0 0 0 0 261934 0 0 3 3 1 3 3 5 2 1 0 0 0 301935 0 0 8 1 1 1 2 1 0 7 2 1 1 0 0 521936 1 0 2 14 7 2 0 1 0 0 0 0 271937 0 0 5 3 3 1 2 1 1 0 0 0 161938 0 0 3 1 4 8 3 0 2 0 0 0 0 301939 0 0 2 11 23 5 1 2 0 1 1 0 461940 0 0 7 1 1 1 8 1 2 4 0 0 0 0 0 521941 0 0 6 7 1 4 7 5 0 0 0 0 0 391942 1 0 2 5 15 4 3 0 1 1 0 0 321943 1 0 0 13 14 0 4 2 1 1 0 0 361944 2 0 4 9 15 9 3 1 1 0 0 0 441945 0 0 2 9 6 3 1 0 0 0 1 0 221946 0 0 1 6 9 3 1 0 0 0 0 0 201947 0 0 7 5 6 2 1 1 1 0 0 0 231948 0 0 13 12 3 4 1 1 2 0 0 0 411949 0 0 8 22 6 0 0 1 0 1 0 0 381950 2 0 5 16 3 3 0 0 0 0 0 0 29(continued )
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Historical SeismogramsandEarthquake
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ToJames F. Landerfor his leadership
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viContentsThe Status, Importance, a
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...VlllEarthquake History of Califo
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XMicrofilming of Historical Seismog
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PrefaceA symposium on Historical Se
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I. Introduction
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4 W. H. K. Lee, H. Meyers, and K. S
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6 W. H. K. Lee, H. Meyers, and K. S
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8 W. H. h‘. Lee, H. Meyers, and K
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10 W. H. K. Lee, IT. Meyers, and K.
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12 W. H. K. Lee, H. Meyers, and K.
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14 W. H. K. Lee, H. Meyers, and K.
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IMPORTANCE OF HISTORICAL SEISMOGRAM
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18 Hiroo KanamoriTable Ib. Some Lar
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-60'1 1904-1985-M, >8.01II\I'.iPlus
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22 Hiroo Kanamorievents often have
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~~~24 Hiroo KanamoriThatcher et al.
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26 Hiroo Kanamo riIf relatively com
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28 Hiroo Kanamori9. Difficulties in
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30 Hiroo KanamoriNagamune, T. (1971
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32 Hiroo KanamoriI I I I I1000100z
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11. Analysis of Historical Seismogr
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38 Kat su y uki A beaddition to thi
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42 Katsuyuki Abe20:oow19:302-I--Ia
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44 Katsuyuki AbeIn the present stud
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46 Katsuyuki AbeTable 3. Sinkiang E
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~48 Katsuyuki AbeSieh (1978) and ot
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50 Katsuyuki AbeREFERENCESAbe, K. (
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52 E. Hurtig and G. KowalleFRG'.L.-
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54 E. Hurtig and G. Kowalle2.2 Reco
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56 E. Hurtig and G. KowalleREFERENC
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58 N. V. Kondorskaya and Yu. F. Kop
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THE STATUS, IMPORTANCE, AND USE OFH
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66 Ota Kulhdnek1 8 35lo. r 1s ' 20
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68 Ota Kulhdnek1 UPP EW SEP 9 1954
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ANALYSIS OF HISTORICAL SEISMOGRAMS
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72 S. K. Singhfrom Uppsala. We also
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74S. K. SinghN1 1Oaxaca-X .-x x- x
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76S. K. SinghESKUPPWIECHERT ELPZ A-
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78 S. K. SinghJdFJ-22 Feb 1943Ms=7.
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80 S. K. SinghDE BlLT (DBN) Z$I = 3
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82 S. K. Singh7. The Great Jalisco,
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84 S. K. SinghREFERENCESAbe, K. (19
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86 S. Stein, E. A. Okal and D. A. W
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94S. Stein, E. A. Okal and D. A. Wi
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96S. Stein, E. A. Okal and D. A. Wi
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100 S. Stein, E. A. Okal and D. A.
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RECENT ACTIVITIES AT THE INTERNATIO
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S.S. Felt and Damaging EarthquakesI
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In t e r na tio n a1 Se is mo logic
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1. IntroductionCatalogue of Chinese
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Catalogue of Chinese Earthquakes (M
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Catalogue of Chinese Earthquakes (A
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Catalogue of Chinese Earthquakes (A
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DATA BASES ON HISTORICAL SEISMICITY
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Data Bases on Historical Seismicity
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COMPILATION AND PROCESSING OF HISTO
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Compilation and Processing of Histo
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The U. S. Geological Survey’s Dat
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The U. S. Geological Survey's Datab
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~ ~The U. 5‘. Geological Survey
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The U. S. Geological Survey’s Dat
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Catalog of Large and Damaging Earth
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YCatalog of Large and Damaging Eart
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YM D h m1918 2 9 20 461918 2 13 6 7
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His to ric al Mate ria Is of Chine
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Historic a1 Mate rials of Chinese E
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Historical Materials of Chinere Ear
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His t o r ical Mate rials of Chin e
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IV. Individual Historical Earthquak
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174 N. N. Ambraseys and C. F. Finke
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182 N. N. Arnbraseys and C. P. Melv
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184 N. N. Ambraseys and C. P. Melvi
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188 N. N. Arnbraseys and C. P. Melv
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202G. E. Fiedler B.FI1 IFigure 1. T
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204 G. E. Fiedler B.Figure 3. The S
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206 G. E. Fiedler B.Origin time Epi
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EVALUATION OF DAMAGE AND SOURCE PAR
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2 10 D. Muiioz and A. Udias3. Evalu
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212 D. Muiioz and A. Udias3 wFigure
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2 14 D. Mun"oz and A. Udiasgiven by
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216 D. Muioz and A. UdiasTable 2. D
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218 D. Munot and A. UdiasGentil, P.
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220 D. Muiioz and A. UdiasArchivo M
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V. Earthquake History
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226 M. DeBecker and T. CamelbeeckAt
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~~228 M. DeBecker and T. Camelbeeck
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230 M. DeBecker and T. Camelbeeek10
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DOCUMENTING NEW ZEALAND EARTHQUAKES
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234 G. A. EabyFrom a seismic point
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236 G. A. EibyImmediate practical p
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238 G. A. Eibynorth-west; but subsi
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240 G. A. Eibywith near-earthquake
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242 Pao Hua Lee120 121 122 123Figur
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0.3244 Pao Hua Lee(3) Ryukyu-Taiwan
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Pa0 Hua LeeTable 2. Major Earthquak
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248 Pao Hua LeeTable 2. (Continued
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250 Pao Hua Lee‘. . . an earthqua
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252 Pao Hua LeeREFERENCESCentral We
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254 S. Prac h ua b21I151 O0IFigure
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256 S. PrachuabTable 1. 12 Seismic
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258 S. Prac h u a bTable 2. (Contin
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260S. Prachuab94" 96" 98" 1 ooo2ac2
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262 S. Prachuab.17 MAY 1955EMrliCUA
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:;13264 S. Prachuab0 .me.0 . .eeee0
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266 S. Prac hua b005 6 7MAGNITUDEFi
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268 T. R. Toppozada, C. R. Real, an
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270 T. R. Toppozada, C. R. Real, an
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2 72 T. R. Toppozada, C. R. Real, a
Page 288 and 289: 274 T. R. Toppozada, C. R. Real, an
Page 290 and 291: STUDY OF HISTORICAL EARTHQUAKES IN
Page 292 and 293: 278 Tatsuo Usarni(3) Documents publ
Page 294 and 295: 280 Tatsuo Usarnin5nlob0D KyotoKama
Page 296 and 297: 282 Tatsuo Usami:.:.., ........ L,/
Page 298 and 299: 284 Tatsuo Usami(2) A tsunami attac
Page 300 and 301: 286 Tatsuo Usami1897lntenrLFigure 6
Page 302 and 303: ~ ~~~~288 Tatsuo UsamiTable 4. Occu
Page 304 and 305: 290 R. G. Valenzuela and L. C. Garc
Page 306 and 307: n09n08n001NoZlNobIn091n081N 002
Page 308 and 309: ~ ~~294 R. G. Valenzuela and L. C.
Page 310 and 311: 296 R. G. Valenzuela and L. C. Garc
Page 312 and 313: 298 R. Muir Wood, G. Woo, and H. Bu
Page 323 and 324: MAGNITUDE-FAULT LENGTH RELATIONSHIP
Page 325 and 326: APPLICATIONS OF FUZZY MATHEMATICSIN
Page 327 and 328: Applications of Fuzzy Mathematics 3
Page 333 and 334: Applications of Fuzzy hluthematics
Page 335 and 336: ON THE SEISMICITY OF THE MIDDLEASTS
Page 337: uca,m a,kma,.IY kfi30 uhd
Page 341 and 342: On the Seismicity of the Middle Eas
Page 347 and 348: On the Seismicity oj the Middle Eas
Page 349 and 350: HISTORICAL SEISMICITY AND EARTHQUAK
Page 351 and 352: Historical Seismic it y and Earthqu
Page 353 and 354: fIistorica1 Seismicity and Earthquu
Page 355 and 356: Historical Seismicity and Earthquak
Page 363 and 364: PATTERN ANALYSIS OF SMALL EARTHQUAK
Page 365 and 366: Pattern Analysis of Small Earthquak
Page 377 and 378: Earthquakes and Deep Fracture Zones
Page 379 and 380: --_-Earthquakes and Deep Fracture Z
Page 381 and 382: Earthquakes and Deep Fracture Zones
Page 383: Earthquakes and Deep Fracture Zones
Page 387 and 388: HISTORICAL SEISMOGRAM FILMING PROJE
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~~Historical Seismogram Filming Pro
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Historical Seismogram Filming Proje
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Historical Seismogram Filming Proje
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Filming Seismograms and Related Mat
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Digitization and Processing of J.M.
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SOME REMARKS ON HISTORICAL SEISMOGR
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Historical Seismograms and the Micr
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~~~~Historical Seismograms and the
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His torical Se is mogru ms and the
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Historical Sezs mogra ms and the Ma
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H1s t o rical Seismograms a nd the
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Historical Seismograms in China 42
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424 Kezin Qua History of Chinese Se
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428 Kexin Qu8. Plans for the Near F
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430 0. Ye. Starovoita station, its
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DAT ANDTHE STANDARDIZATION OF SEISM
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434 Y. Tamura, H. Sasaki, M. Ooe, a
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~ So.i436 Y. Tarnura, H. Sasaki, M.
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438 Y. Tarnura, H. Sasaki, M. Ooe,
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440 Yasuhiro Umeda and Katsuyoshi I
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442 Yasuhiro Umeda and Katsuyoshi I
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HISTORICAL SEISMOGRAMS IN ITALYR. C
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Historical Seismograms in Italy 449
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HISTORICAL SEISMOGRAMS FROM AUSTRAL
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His to rical Se is mog ra ms From A
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SEISMOGRAMS MADE BEFORE 1963 AT STA
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2. New ZealandSeismograms Before 19
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Seismograms Before 1963 in the Sout
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Seismograms Before 1963 in the Sout
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Historical Seismograms Recorded in
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Hist orieal Se is mograms Reeo rded
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THE HISTORICAL SEISMOGRAMS OF COLOM
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The Historical Seismograms of Colom
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Helwan Historical Seismograms 475Al
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Se is mo log ic a1 Mea s use me n t
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Seismological Measurement an Hong K
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A BRIEF HISTORY OF THE SEISMOLOGICA
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History of the Seismological Observ
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~~ ~ ~ ~~ ~ ~~Historical Seismogram
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494 Sergio S. Su, S. J.Figure S. Se
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496 Sergao S. Su, S. J.Figure 7. Ce
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498 K. L. SuendsenDominican Republi
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INDEXAAbuyama Seismological Observa
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Index 503China, see also Taiwan466
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Indez505HIHalin seismograph, 421Haw
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Index 507Karuizawa, 417Kobe, 117, 1
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Index 509PPacific Ocean1943 Malpelo
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Index 511Sri Lanka, Colombo station
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Index 513Wood-Anderson seismographW
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