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

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136 A. D. Gvishiani and Wilbur A. Rinehartk -NUMBER OF ERROR RECORDS BEFORE CORRECTION PROCESSPi -PROBABILITY TO FIND AN ERROR IN THE ith VERIFICATION, i=l, 2ni -NUMBER OF DISCOVERED ERRORS IN THE ith VERIFICATION, i=l, 2n -NUMBER OF DISCOVERED ERRORS IN BOTH VERIFICATIONSPROBABILITY OF THE EXISTENCE OF AN ERROR IN THE VALUE OF THEPARAMETER AFTER THE VERIFICATION PROCESSq = 1 -PI -P2+P1P2WITH THE PROBABILITYP(!) = CkP qf (l-q) k-!WHERECkp = k(k-1). . . . . . . . . . (k-f +1)f !FOR k‘ ERRORS IN THE FILEFigure 6. Estimation of the probability of an error after data base correction.According to the method represented in Figure 6, Gvishiani and Zheligovsky (inpress) obtained a 90% probability that the number of erroneous records in the file(which currently contains more than 7,000 strong earthquakes in the territory ofthe USSR) is not higher than 10. This number of errors, which is small comparedto the size of the file, is unusually small for computer-readable catalogs.3. ApplicationsThe main goal of creating the seismological data bases in NGDC and IPE is toprovide data for scientific and engineering research and for development of worldwideand regional epicenter maps.The number of users of NOAA and IPE data bases increases each year. Thedata from computer-readable earthquake catalogs are widely used in scientific andengineering research. An important example of such scientific application of theNOAA and IPE data bases is evidenced by the recognition of areas prone to strongearthquakes. In this research, as objects of recognition, we recognize the morphostructuresnear which strong earthquake epicenters are a priori clustered. Usingthe descriptions of these objects as geological and geophysical parameters, patternrecognition algorithms make an attempt to answer the question: “Is a strong earthquakepossible in the vicinity of the given object?” Strong earthquakes are thoseof magnitude larger than a chosen threshold M 2 M,, where M, depends on theterritory under consideration.
Data Bases on Historical Seismicity1370-86LEGENDDongerous Areas00mPI =U....Non-Dangerous Areas ....Ins tr u men tal Earthquakes 0Recent Earthquakes locations +Cwere predicted by patternrecognition methods.90 0 90 100 h11mt-t--rA-7-1I \ 0 :'I80 73 .-Figure 7. Pacific coast of South America where recent earthquake locations werepredicted by pattern recognition methods.243240
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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
Page 100 and 101: 86 S. Stein, E. A. Okal and D. A. W
Page 108 and 109: 94S. Stein, E. A. Okal and D. A. Wi
Page 110 and 111: 96S. Stein, E. A. Okal and D. A. Wi
Page 114 and 115: 100 S. Stein, E. A. Okal and D. A.
Page 121 and 122: RECENT ACTIVITIES AT THE INTERNATIO
Page 123 and 124: S.S. Felt and Damaging EarthquakesI
Page 125 and 126: In t e r na tio n a1 Se is mo logic
Page 127 and 128: 1. IntroductionCatalogue of Chinese
Page 129 and 130: Catalogue of Chinese Earthquakes (M
Page 135 and 136: Catalogue of Chinese Earthquakes (A
Page 139 and 140: Catalogue of Chinese Earthquakes (A
Page 145 and 146: DATA BASES ON HISTORICAL SEISMICITY
Page 147 and 148: Data Bases on Historical Seismicity
Page 149: Data Bases on Historical Seismicity
Page 153 and 154: COMPILATION AND PROCESSING OF HISTO
Page 155 and 156: Compilation and Processing of Histo
Page 157 and 158: The U. S. Geological Survey’s Dat
Page 159 and 160: The U. S. Geological Survey's Datab
Page 161 and 162: ~ ~The U. 5‘. Geological Survey
Page 163 and 164: The U. S. Geological Survey’s Dat
Page 165 and 166: Catalog of Large and Damaging Earth
Page 167 and 168: YCatalog of Large and Damaging Eart
Page 171 and 172: YM D h m1918 2 9 20 461918 2 13 6 7
Page 177 and 178: His to ric al Mate ria Is of Chine
Page 179 and 180: Historic a1 Mate rials of Chinese E
Page 181 and 182: Historical Materials of Chinere Ear
Page 183 and 184: His t o r ical Mate rials of Chin e
Page 185: IV. Individual Historical Earthquak
Page 188 and 189: 174 N. N. Ambraseys and C. F. Finke
Page 196 and 197: 182 N. N. Arnbraseys and C. P. Melv
Page 198 and 199: 184 N. N. Ambraseys and C. P. Melvi
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180 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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2 72 T. R. Toppozada, C. R. Real, a
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STUDY OF HISTORICAL EARTHQUAKES IN
Page 292 and 293:
278 Tatsuo Usarni(3) Documents publ
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280 Tatsuo Usarnin5nlob0D KyotoKama
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282 Tatsuo Usami:.:.., ........ L,/
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284 Tatsuo Usami(2) A tsunami attac
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286 Tatsuo Usami1897lntenrLFigure 6
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~ ~~~~288 Tatsuo UsamiTable 4. Occu
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290 R. G. Valenzuela and L. C. Garc
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n09n08n001NoZlNobIn091n081N 002
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~ ~~294 R. G. Valenzuela and L. C.
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296 R. G. Valenzuela and L. C. Garc
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298 R. Muir Wood, G. Woo, and H. Bu
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MAGNITUDE-FAULT LENGTH RELATIONSHIP
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APPLICATIONS OF FUZZY MATHEMATICSIN
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Applications of Fuzzy Mathematics 3
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Applications of Fuzzy hluthematics
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ON THE SEISMICITY OF THE MIDDLEASTS
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uca,m a,kma,.IY kfi30 uhd
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On the Seismicity of the Middle Eas
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On the Seismicity oj the Middle Eas
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HISTORICAL SEISMICITY AND EARTHQUAK
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Historical Seismic it y and Earthqu
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fIistorica1 Seismicity and Earthquu
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Historical Seismicity and Earthquak
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PATTERN ANALYSIS OF SMALL EARTHQUAK
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Pattern Analysis of Small Earthquak
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Earthquakes and Deep Fracture Zones
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--_-Earthquakes and Deep Fracture Z
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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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Page 489 and 490:
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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