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

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266 S. Prac hua b005 6 7MAGNITUDEFigure 10. The relation between magnitude and mean return period.REFERENCESBender (19.83). Geology of Burma, Gebruder Borntrayer, Berlin, 293 pp.Fontaine, H. and D. R. Workman (1978). Review of the geology and mineral resourcesof Kamphuchea, Laos and Vietnam, Reg. Conf. Geol. Miner. Resour. Southeast AsiaProc., 3, 539-603.Gutenberg, B. and C. F. Richter (1954). Seismicity of the Earth and Related Phenomena,Princeton Univ. Press, 310 pp.Hattori, S (1974). Regional distribution of b-value in the world, Znf. Znst. Seismol. EarthquakeEng. Bull., 12, 39-57.Nutalaya, P. and S. Sodsri (1983). Seismicity Data of Thailand and Adjacent Areas, AsianInst. Tech., Bangkok, Thailand, Al-A5, B1-B109, Cl-C5.Nutalaya, P. and S . Sodsri (1984). Seismic Source Zones and Earthquakes Recurrence Relationshipof the Burma- Thailand-Zndochina Area, Asian Inst. Tech., Bangkok, Thailand,1-46.Utsu, T. (1967). Some problems of the frequency distribution of earthquakes in respect tomagnitude (I), Geophys. Bull. Hokkaido Uniu., 18, 53-69.Welkner, P. M. (1965). Statistical analysis of earthquakes occurrence in Japan, Znt. Znnst.Seisnol. Earthq. Eng. Bull., 2, 1-27.Win Swe (1980). A major Strike-Slip Fault in Burma, 1, 63-72 (presented at The FifthBurma Research Congress, 1970, Revised and title changed, 1980).
1. IntroductionEARTHQUAKE HISTORY OF CALIFORNIAT. R. Toppozada, C. R. Real, and D. L. ParkeCalifornia Department of ConservationDivision of Mines and Geology690 Bercut Drive, Sacramento, CA. 95814, USAThe history of earthquake occurrences is basic to assessing and mitigating earthquakehazards. Statewide seismographic coverage in California was established in1932. Before 1932, the record of earthquakes comes from the effects reported by thepopulation. Interpretation of the pre-instrumental record provides the approximatelocation and sizes of earthquakes. Because the pre-instrumental record covers alonger period than the instrumental record, it includes a major proportion of thelarge earthquakes, which are rare events.The earthquake history shows what the strongest earthquake effects have beenin various parts of the state. Critical structures such as nuclear power plants,dams, and hospitals are then designed to withstand at least these historical effects.The earthquake history also suggests the location of seismically active fault zones.If further geological study of these faults shows that they were active during theHolocene (last 10,000 years), they are zoned so that structures are not built onactive fault traces.The rate of occurrence of earthquakes in various fault zones, when combined withgeologic and geodetic rates of deformation, helps to define the recurrence interval ofdestructive earthquakes in these zones. The fault zones that are most likely to rupturein the near future are then selected for the development of emergency responseplans, and for the concentration of earthquake prediction monitoring efforts.2. Completeness of the RecordThe written history of damaging California earthquakes begins in 1800, whenthe first earthquake damage was reported at Mission San Juan Bautista. From thattime on, earthquakes were reported only if they were damaging (Modified Mercalliintensity VII or greater) at any of the missions, which were located along the coastin central and southern California. Thus, the record is probably complete backto 1800 only for earthquakes of about magnitude 7 (M7) or greater that occurredwithin 70 km of the coast south of San Francisco.Newspaper coverage came to California with the 1849 gold rush. Newspapersreported earthquake felt effects as well as damage effect. During the 1850’s, 1860’s,and 1870’s, newspaper coverage was concentrated around San Francisco Bay andin the gold mining area east of Sacramento, with limited coverage along the coast.Thus, from 1850 the record is probably complete for earthquakes of about A4 6or greater around San Francisco Bay and in the gold country. From 1850-1880,in other areas of California the record is probably complete only for M7 or largerearthquakes. After 1880, with the increase of newspaper coverage, the statewiderecord of earthquakes is probably complete for events of M6 or greater. Starting inthe early 1900’s, with the advent of statewide seismographic recording, the recordis complete for M6 or greater earthquakes.Historical Seismogramsand Earthquakes of the World267Copyright 1C IO8X by Academic Press, Inc.All rights of reproduction in any form reserved.
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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
Page 230 and 231: 216 D. Muioz and A. UdiasTable 2. D
Page 232 and 233: 218 D. Munot and A. UdiasGentil, P.
Page 234 and 235: 220 D. Muiioz and A. UdiasArchivo M
Page 237: V. Earthquake History
Page 240 and 241: 226 M. DeBecker and T. CamelbeeckAt
Page 242 and 243: ~~228 M. DeBecker and T. Camelbeeck
Page 244 and 245: 230 M. DeBecker and T. Camelbeeek10
Page 246 and 247: DOCUMENTING NEW ZEALAND EARTHQUAKES
Page 248 and 249: 234 G. A. EabyFrom a seismic point
Page 250 and 251: 236 G. A. EibyImmediate practical p
Page 252 and 253: 238 G. A. Eibynorth-west; but subsi
Page 254 and 255: 240 G. A. Eibywith near-earthquake
Page 256 and 257: 242 Pao Hua Lee120 121 122 123Figur
Page 258 and 259: 0.3244 Pao Hua Lee(3) Ryukyu-Taiwan
Page 260 and 261: Pa0 Hua LeeTable 2. Major Earthquak
Page 262 and 263: 248 Pao Hua LeeTable 2. (Continued
Page 264 and 265: 250 Pao Hua Lee‘. . . an earthqua
Page 266 and 267: 252 Pao Hua LeeREFERENCESCentral We
Page 268 and 269: 254 S. Prac h ua b21I151 O0IFigure
Page 270 and 271: 256 S. PrachuabTable 1. 12 Seismic
Page 272 and 273: 258 S. Prac h u a bTable 2. (Contin
Page 274 and 275: 260S. Prachuab94" 96" 98" 1 ooo2ac2
Page 276 and 277: 262 S. Prachuab.17 MAY 1955EMrliCUA
Page 278 and 279: :;13264 S. Prachuab0 .me.0 . .eeee0
Page 282 and 283: 268 T. R. Toppozada, C. R. Real, an
Page 286 and 287: 2 72 T. R. Toppozada, C. R. Real, a
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 329 and 330: Applications of Fuzzy Mathematics 3
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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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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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