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

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364 J. Vani'k and V. Hanu;In Ecuador, eight fracture zones of this type were delineated. The basic scheme ofthese fracture zones is given in Figure 2, which shows their position on the surfaceas determined by the shallowest earthquakes associated with the correspondingfracture zone. The most important parameters of the individual fracture zones aregiven below. Complete graphical documentation can be found in Hand and VanPk(1987b); here, as an example, only sections for fracture zones KO, KIN, and K2Nare shown (Figure 3).(1) Otavalo-Umpalh fracture zone (F)Outcrop position: (0.10' S, 79.15' W), (0.50' S, 78.65" W) - (7.15" N, 73.05' W),(6.70" N, 72.55" W); length of the active part: 1050 km; width on the surface: 70km; dip 44' to southeast; maximum depth of associated earthquakes: 135 km.(2) Pelileo-Zuiiac fracture zone (KO)Outcrop position: (1.00' S, 78.60' W), (1.00'' S, 78.30' W) - (2.50" S, 78.60' W),(2.50' S, 78.30'' W); length 165 km; width 30 km; dip 39" to west; maximum depth70 km.(3) Puyo-Yaupi fracture zone (KlN)Outcrop position: (1.05' S, 78.05' W), (1.05' S, 77.70' W) - (2.90' S, 78.05' W),(2.90' S, 77.70' W); length 210 km; width 40 km; dip 38' to west; maximum depth85 km.282W 80 76I024:I I I rFigure 2. Scheme of seismically active fracture zones in Ecuador. Axis of the Peru-Chile trench is denoted by a serrated line.
--_-Earthquakes and Deep Fracture Zones an Ecuador 36581W 80 79 70 8OW 79 70 35 2 11Ijl+ev23s L."00W179 70 7723s;.p' km100IU 20079W 78 77, 35 2 I79W 70 77 7679W 70 77 35 2 1km100200Figure S. Location (a) of the Pelileo-Zuiiac fracture zone (KO), the Puyo-Yaupi fracturezone (KIN) and the Tihuano-Huasaga fracture zone (K2N) with their associatedearthquakes, cross-sections perpendicular to (b) and parallel to (c) the corresponding fracturezone. Symbols of earthquakes as in Figure 1.(4) Tihuano-Huasaga fracture zone (K2N)Outcrop position: (1.25' S, 77.40' W), (1.25" S, 77.05' W) - (2.95' S, 77.40' W),(2.95' S, 77.05' W); length 185 km; width 40 km; dip 41' to west; maximum depth80 km.(5) Mancora-Rio Huitoyacu fracture zone (U)Outcrop position: (3.90' S, 81.26' W), (4.30' S, 81.20' W) - (3.12' S, 76.93' W),(3.55' S, 76.84' W); length 490 km; width 45 km; vertical fault; maximum depth130 km.(6) Esmeraldas-Rio Curaray fracture zone (EC)Outcrop position: (1.65' N, 80.10" W), (1.30' N, 80.40' W) - (1.10' S, 76.80' W),(1.40' S, 77.10' W); length 475 km; width 50 km; dip 47' to northeast; maximumdepth 130 km.
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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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2 72 T. R. Toppozada, C. R. Real, a
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STUDY OF HISTORICAL EARTHQUAKES IN
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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
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
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Page 339 and 340: 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: Earthquakes and Deep Fracture Zones
Page 381 and 382: Earthquakes and Deep Fracture Zones
Page 383: Earthquakes and Deep Fracture Zones
Page 387 and 388: HISTORICAL SEISMOGRAM FILMING PROJE
Page 389 and 390: ~~Historical Seismogram Filming Pro
Page 391 and 392: Historical Seismogram Filming Proje
Page 393 and 394: Historical Seismogram Filming Proje
Page 395 and 396: Filming Seismograms and Related Mat
Page 405 and 406: Digitization and Processing of J.M.
Page 415 and 416: SOME REMARKS ON HISTORICAL SEISMOGR
Page 417 and 418: Historical Seismograms and the Micr
Page 421 and 422: ~~~~Historical Seismograms and the
Page 425 and 426: His torical Se is mogru ms and the
Page 427 and 428: 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 and the Micr
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Historical Seismograms and the Micr
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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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