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130 published in the same format as that of the original catalog. Some epicenters and other parameters, already published, may be modified by later studies and these new values will be published in the hRevista Brasileira de Geo fs ica. ADDITIONAL REFERENCES: See page 28.
INTRODUCT I ON 131 CATALOC OF EARTItQUAES FOR CHILE HYPOCENTER AND INTENSITY DATA NATIONAL REPORT Edgar Kuasel Th, Cat alog of EaLirthquakes has a long history in Chiie. Dur:ing the past centLury, several atthors accumulated information on earthivpakes which have occurred in Clile in colonial oime. Generall , those coDila ti:or,.- were retated with studles or ien ,d for Li- preparation of texts on Hlistorv and Geogrniphv of (hile,, ralthei thin for sc:ientific purposes. Cor:ainl., K w:. Io p, tesits hi, IV IIore ( 19 1-19 6) woi ireop red tae most CoMr,1 *¢I -, Cat : of tie his:-torical Wr : ii c .n;t r t: lhqua ks. le greaterl. part of the hi't riv'.l cntalog, which have been pulished lt u':, ae based nn his w umpncah Y..'ark. ;reve (196,) and Lomnit: (197(0) h;ve ,ad n t the work dton-, K , r,.su- do Bhai] l r '- . 1'urt erifl e, severaul int'rn ti inal dl the first loir decades of hr pr Oin rtu nturv , in tiL utions ,nid uinivarsit:i vs began rhe preppratinn of world catalogs w,,ith vilimhle informatioen elated to Chile. Tb',- information on epicentnto rs with instrumnental data has been obtained princi pa ll,,yrrmi theM catalogi of the U.S. Geological Survey, the Internatinal Seisologc&rmi ry (1919,-1959), (;tit enlsr.i and Ri, ' (190'-1952), Internat or.nt l ?_' ,ical( ' YnPtand ro data fom r t e -e 'mel, ig ,c-1 Service of Me l.n ,rsi, Ie -- l)'partm n ore, Ilo an'd Cenp '' -. A gr oup from the 1ottr ir oione - .uis M alyear,l rin hat,(rrivnt o,-, I'F j ti - nu e] and I.k r:o Pn, , Sum ,,o c 0 Chiiitu Wall "esp-nsibip for ri-o"der iuug 11se of thp abov tiit ionei tho dal.Tu i n a new caalo of cart hcu.&our(es ald othetq less important. Th . n c -, ping of intensitis was rpvised bv Luis Alvear and John Bannister, by checi,,g%infor- runt ion i.oinp m i led by d i fferent: authors.s METI!OI)S I'MI1) N IHE PRIRIARAtI(iN OF- THE CATALOGS. lie genecration of the catalogs of hypocenter and :intensities laborious. The material used i.n documented in detail in each o-ne -was5 very : th, references at: the end of this report. Here we will refer Only criteria used to select or adopt t:he liyp ocent ral parameters. cO .-W ,,tu O tif For the historical earthquakes (non-inst rtl~ntma) , the epicnurn coordinates corr'espond to the coordinates of tihe gogralphic locality; h- i:hlthe earthquake is known (city , town , ItmaV be errors of F 2" i t o o t. tti , etc.). Ti- exp.ains why -!. of- -one of the e 'ronts. +7!*;: r Iod,' of those earthquas r ir er-spond to " us tinted I', on K hf :-'' iacroseisinic itnformiltion nal vred by Lonm itz (1970) and I iiu ci (1979r). "''. ro&d used for tihe ma gn i tnlde ,sCaI e , in :;uch caseps, r' i s E (column 92 ) . ,h,- r... authors have est inlat oil a rai.ge of" l851,itiides , the inmein of thS rane to tlie nearest utppe r decimal point . The information concerning the m15- used time of giin w:s olbtained from a compilation by Barrientos (198!) (;1T. and coosvcrte.T t:o
Page 1 and 2:
Centro Regional de Sismologfa para
Page 3 and 4:
Este trabajo se publica con el ente
Page 5 and 6:
INDICE - CONTENTS DESCRIPCION DEL C
Page 7 and 8:
Pals Coordinador Investigadores 2 R
Page 9 and 10:
'4 Todas Ias intensidades 1istndas
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individuales. Esto requiriA definir
Page 13 and 14:
8 mb = log (A/T) + 1.35 log (A ) +
Page 15 and 16:
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
Page 27 and 28:
23 A 0 ML = lig A/T + 1.9 log + 3.5
Page 29 and 30:
25 A partir de 1982 los datas sismi
Page 31 and 32:
27 m) = 1.63 + 0.60 Jog (At), 6 i b
Page 33 and 34:
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
Page 45 and 46:
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
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fuente du a"lorl;a B; (tp ignaJ~l m
Page 61 and 62:
)'''n4'Va,!o "IN't; MK3, n importtn
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59 I so ejemplifican algunos tomado
Page 65 and 66:
a"lt or i6 at Ias' primrdB JleM ros
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DESCRIPCION DIE ENT RADA.; IV,N , C
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APFICE1 f A (CihnL inaari 'Si) (>I
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APENDICE A (Continuacj6n) Columna r
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APENDICE B (Continu cin) Co ,,_ i t
Page 75 and 76:
Tipa do Hlypocent:ro V.digo SISRA T
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' ipo de Cd igo Ilypocentro STSRA n
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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 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: 129 mb = 1.63 + 0.60 log(A t), or m
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
Page 167 and 168: I 63 APPENUITX 11 (Continued) Colum
Page 169 and 170: Type of' Hyuoeenter I n 3 t r u m e
Page 171 and 172: 10 7 TABLE 3--.DEPT!H QUALITY FACTO
Page 173 and 174: 'rAILE 4--(Contlnued) EDR Earthquak
Page 175 and 176: i I I TABLE 4--- (Continued) MOL Mo
Page 177 and 178: TABLE 4--(Continued) Wt3 Bachmann,
Page 179 and 180: t 75 TABLE 5--Continued JGG Grases,
Page 181 and 182: I i7/ TABLE 6--MAGNITUDE SCALE CODE
Page 183 and 184: IILBV P. liuaco, W. Lescano, A. Buo
Page 185 and 186:
TRMl Trinidad Station, Trinidad, We
Page 187 and 188:
211 larrington, I.j., 1944, Volcano
Page 189 and 190:
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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