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

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kilometer. The mb and M s magnitudes listed in the hypocenter catalog are 110 repeated in the intensity catalog. Space is included to report up to three different maximum intensities. The first is the observed maximum intensity. This is the actual maximum value of all reported intensity observations. In some situations, however, an intensity may not be reported at a location where the maximum intensity occurred. This may happen if the epicenter of the event is offshore or located in an unpopulated area. In these situations it is often possible to estimate what the maximum intensity would have been based on the distribution of other observed intensities. Thus, the second maximum intensity included is an estimated maximum. The third is a maximum intensity computed from a reported magnitude using an appropriate regression formula. The last value in the hypocenter record indicates the number of location records which follow. Each location record describes an observed intensity value for a given location. A two-letter country code is listed to indicate the country in which the intensity was reported. A description of the locality is given, which is usually the name of a city or village sometimes followed by the province in which it is locaLed. Sometimes the country name is again included in this description. Coordinates and elevation of the location are listed. Space is provided to report the distance from the epicenter to the location and the distance from the hypocenter to the location. The difference between these two parameters is that the hypocenter distance takes into account depth of the hypocenter and elevation at the given location while the epicentral distance does not. Space is also provided to report the azimuth between the czicenter and the coordinates of the given location. The observed intensity for that location is listed. All intensities are identified with the scale used for evaluation, either Modified Mercalli or MSK. The investigator who
assigned the iJntonnsity value is also identified under "Interpreter". Uo to four references are listed. Tho.se are references to published material, which may include assigned intenslty vaJues or may be only descriptions of damage frow an event. Baned on there references the interpreter has assigned an Antensity value fop that location. A column is also provided for comments relating to that .cation. Thin space may be used to point out unusual oasnoss for damage such as iqufaction or landslides. The hypocentral parameters givn in the intensity catalog are the same as those li3ted in the hyponter catalog. This is important because no references are provided for the hyponentral data included in the intensity catalog, but these refcrercumay be found by referring back to the hypocenter catalog. It is also eusent.al that the identifying number used In the intensity catalo.g correspond with the number in the hypocenter catalog and that any event given in the intensity catalog be included in the hypocenter catalo;. During the compilaLion of the Intensity catalog we have attempted to insure that; this correspondence is maintained. Some question arose as to what the maximum intensity in the hypocenter catalog represents. Should this necessarily correspond to the maximum intensity ,iven in the intensity catalog, and if so which of the three possible maximum intensities? During the compilation, we have checkea that the maximum observed intensity given in the intensity catalog is the actual maximum of the reported intensity otser'vations. Maximum intens ties listed in ,v h.'ceenter catalog may differ' fCom those listed In the intensity catalog. in order- to provide thn best estimate possible of the stze of historical events, the hypocenter o;ta]og may list an estimated maximum Intensity. This .s most likely in th case of offshore events.
Page 1 and 2:
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
Page 17 and 18:
Conclusiones 12 Los catilogos unifi
Page 19 and 20:
Introducci6n 15 CATALOGO DE TERREMO
Page 21 and 22:
17 Los criterios de selecci6n de ev
Page 23 and 24:
4. Torremoto Stdin .i Cl ino del 3)
Page 25 and 26:
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. &
Page 35 and 36:
A Ia colmna 131 (WFn6munus s -t , n
Page 37 and 38:
3 KAUSEI,, E. (1979d). Terremoto do
Page 39 and 40:
INTRODUCCION .'5 CATAIO(;O DE .1ElI
Page 41 and 42:
37 se pretendla adem~s elaborar lis
Page 43 and 44:
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
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7. Io t ermi i (i ojliiao s i dad !
Page 51 and 52:
INTRODUCC1ON 47 CA'ALOOI ) I)t.E TF
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4Q) ciertos recientes evento:s gi a
Page 55 and 56:
INTRODUCCION CATALOGO DiE TEi,;RNI,
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la interpretaci6n de descripciones
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fuente du a"lorl;a B; (tp ignaJ~l m
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)'''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 and 100: 9 5 REFI EN(CI AS CITADAS Bath, M.,
Page 101 and 102: Introducti on 97 SOUTH AMERICAN HYP
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: intensities but also the distributi
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
Page 151 and 152: 47 in thu conmpiliation presunted a
Page 153 and 154: ii) Every evnl or : Bra:zeo, and fo
Page 155 and 156: is adopted. where: 151 From the equ
Page 157 and 158: 153 TAB IF N ° INTENSITY OBSERVATI
Page 159 and 160: V n u la (1971; 107'); The 'imes At
Page 161 and 162: 11 / A 1'P!' I')IX A DESCIIlPTION O
Page 163 and 164: APPEYN X A (Continued) Columns Head
Page 165 and 166:
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.,
Page 193 and 194:
I8H9 916 "'El Naciuta'l", (Pt ri 1i
Page 195:
191 Needham, R., ard Steele, A., 19
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