catalogo de terremotos para america del sur catalog of earthquakes ...

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96 Needham, R., and Steele, A., 1969, Montana LASA data analysis techniques: S 110-33, Ford Aerospace and Communications, Billings, Mont., 26 p. Ocola, L., Catalogo de intensidades macrosismicas del Peril, 11171-1981, Memoria Explicativa, 1984, Macroseismic hypocenters of Bolivia - Colombia - Ecuador - PerO, 1471-1981: Instituto Geofisico del Pero, Lima, Pero, in preparation. Silgado F.E., 1985, Destructive earthquakes of South America 1530-189'I: Earthquake Mitigation Program in the Andean Region, vol. 10, CERESIS, Lima, Peru. U.S. Defense Mapping Agency, Political map of South America: North and south sheets, 1:5,000,000, Series 1106, Edition 4. Wood, H.O., and Neuman, F., 1931, Modified Mercalli intensity scale of 1931: Seismological Society of America Bulletin, v. 21, p. 277-283.
Introducti on 97 SOUTH AMERICAN HYPOCENTER AND INTENSITY CATALOGS By Bonny L. Askew and S. T. Algermissen U.S. Geological Survey Denver, Colorado 80225 It has been recognized for some time that a unified catalog of earthquake parameters for South America is essential for progress in many areas of seismological research. Tfils is particularly true for regional studies of seismicity, seismotectonics, and the evaluation of seismic hazards. National catalogs of some of the countries in South America have been available for a number of years and many of these contain data as far back as the 16th century. The quality and scope of the available national catalogs, however, vary from country to country. The "Program for the Mitigation of Earthquake Effects in the Andean Region" (known as project SISRA) provided an unparalleled and perhaps essential framework for an effort to unify the various regional and national earthquake catalogs available. The decision was made early in the project to concentrate work on hypocenter parameters of the earthquakes and on cataloging the distrihut. uf intensity. The essential, and clearly the most important, work on the hypocenter and intensity catalogs was done by a group of national workers within each country. They revised, edited, and integrated the variety of seismicity data available for each country. They then entered the data into a format that had been agreed to by the national representatives from each of the countries. The resulting national catalogs were then reviewed and approved by the national coordinator for the catalogs. Dr. Leonidas Ocola of the Geophysical Institute of Peru served as the overall coordinator for the earthquake hypocenter and intensity
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Centro Regional de Sismologfa para
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Este trabajo se publica con el ente
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INDICE - CONTENTS DESCRIPCION DEL C
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Pals Coordinador Investigadores 2 R
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'4 Todas Ias intensidades 1istndas
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individuales. Esto requiriA definir
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8 mb = log (A/T) + 1.35 log (A ) +
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10 Modificada o MSK. El investigado
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Conclusiones 12 Los catilogos unifi
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Introducci6n 15 CATALOGO DE TERREMO
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17 Los criterios de selecci6n de ev
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4. Torremoto Stdin .i Cl ino del 3)
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INTRODUCCION CATALOG(O DE TE KREMOT
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23 A 0 ML = lig A/T + 1.9 log + 3.5
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25 A partir de 1982 los datas sismi
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27 m) = 1.63 + 0.60 Jog (At), 6 i b
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29 SADOWSKI, G.R.; CSORDAS, S.M. &
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A Ia colmna 131 (WFn6munus s -t , n
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3 KAUSEI,, E. (1979d). Terremoto do
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INTRODUCCION .'5 CATAIO(;O DE .1ElI
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37 se pretendla adem~s elaborar lis
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eA. arclivo del InS.-LAtti) (eolisi
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ESt'ASA-CAI.I'.- ,i, r'pvdia Uni v.
Page 47 and 48:
INTRODUCCION I. Investigadores clab
Page 49 and 50: 7. Io t ermi i (i ojliiao s i dad !
Page 51 and 52: INTRODUCC1ON 47 CA'ALOOI ) I)t.E TF
Page 53 and 54: 4Q) ciertos recientes evento:s gi a
Page 55 and 56: INTRODUCCION CATALOGO DiE TEi,;RNI,
Page 57 and 58: la interpretaci6n de descripciones
Page 59 and 60: fuente du a"lorl;a B; (tp ignaJ~l m
Page 61 and 62: )'''n4'Va,!o "IN't; MK3, n importtn
Page 63 and 64: 59 I so ejemplifican algunos tomado
Page 65 and 66: a"lt or i6 at Ias' primrdB JleM ros
Page 67 and 68: DESCRIPCION DIE ENT RADA.; IV,N , C
Page 69 and 70: APFICE1 f A (CihnL inaari 'Si) (>I
Page 71 and 72: APENDICE A (Continuacj6n) Columna r
Page 73 and 74: APENDICE B (Continu cin) Co ,,_ i t
Page 75 and 76: Tipa do Hlypocent:ro V.digo SISRA T
Page 77 and 78: ' ipo de Cd igo Ilypocentro STSRA n
Page 79 and 80: 71, EGR Egred, J., 1M8, Breve hiq;t
Page 81 and 82: 77 Colombia y en la Cuenca d la Ama
Page 83 and 84: 'FAiLA 5 - tCHDI T ,IA W FUENK:TES
Page 85 and 86: TAG Uniiye rsia IN(( N;wci on.i (.'
Page 87 and 88: 83 TABLA 7 - INTtERPRETES APO Oscar
Page 89 and 90: 711 No not nd. ,.a(~ i n V-npz;o Ia
Page 91 and 92: x / TABA F.- K Fi! N(:IAS 101 Infor
Page 93 and 94: 31i3 lescotes, P.M., and Cahr,', Gc
Page 95 and 96: 422 Polo, J.T., 1904, Sinopsis do t
Page 97 and 98: P.114411 > .iII, 11.Ci'144 1 P . ,
Page 99: 9 5 REFI EN(CI AS CITADAS Bath, M.,
Page 103 and 104: 99' Country Coordinator Investigato
Page 105 and 106: 101 is provided for four, magnitude
Page 107 and 108: S03 These bulletins, for the time s
Page 109 and 110: locally which actually fell in Colc
Page 111 and 112: Brazil: Magn!tudes (mb) were comput
Page 113 and 114: intensities but also the distributi
Page 115 and 116: assigned the iJntonnsity value is a
Page 117 and 118: Shallow: 0-70 kms. S11 Intermediate
Page 119 and 120: 115 compiled, is to more clearly de
Page 121 and 122: INTRODUCTION 117 CATALOG OF EARTHQU
Page 123 and 124: I 9 The criteria for tbe selection
Page 125 and 126: 121 Mendoza: Vil].a Atucl and las t
Page 127 and 128: INTRODUCTION 123 CATALOG OF EARTHQU
Page 129 and 130: 125 M = 1.08 + 0.62 fmx 2. Intensit
Page 131 and 132: 127 and Sternberg (1953) who compil
Page 133 and 134: 129 mb = 1.63 + 0.60 log(A t), or m
Page 135 and 136: INTRODUCT I ON 131 CATALOC OF EARTI
Page 137 and 138: INTRODUCTION 133 CATALOG OF EARTHQL
Page 139 and 140: 1.35 later investigation and for th
Page 141 and 142: t lh, l .'a lua11t-io ,Fi i- t ii.
Page 143 and 144: 1NTRODUCT ION 1. Participating: 139
Page 145 and 146: 7. l)eterminat ion of inten, it rie
Page 147 and 148: ]1 3 sources that appear i the refe
Page 149 and 150: informna tion. For pl;.ce: who.o i
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47 in thu conmpiliation presunted a
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ii) Every evnl or : Bra:zeo, and fo
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is adopted. where: 151 From the equ
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153 TAB IF N ° INTENSITY OBSERVATI
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V n u la (1971; 107'); The 'imes At
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11 / A 1'P!' I')IX A DESCIIlPTION O
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APPEYN X A (Continued) Columns Head
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1,1 APPENDTX A (Continued) Columns
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I 63 APPENUITX 11 (Continued) Colum
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Type of' Hyuoeenter I n 3 t r u m e
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10 7 TABLE 3--.DEPT!H QUALITY FACTO
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'rAILE 4--(Contlnued) EDR Earthquak
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i I I TABLE 4--- (Continued) MOL Mo
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TABLE 4--(Continued) Wt3 Bachmann,
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t 75 TABLE 5--Continued JGG Grases,
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I i7/ TABLE 6--MAGNITUDE SCALE CODE
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IILBV P. liuaco, W. Lescano, A. Buo
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TRMl Trinidad Station, Trinidad, We
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211 larrington, I.j., 1944, Volcano
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185 405 1952, Rmto!; s i,,ivoi 6 gi
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187 436 Espejo, G., y fluaco," P.,
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I8H9 916 "'El Naciuta'l", (Pt ri 1i
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191 Needham, R., ard Steele, A., 19
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