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176 TABLE 5--Continued SCB Observatorio de San Calixto, La Paz, Bolivia. See Lee and Wetmiller (1978) and the text accompanying catalog for a description of magnitude determinations. SIS Project SISAN. See Ocola (1981) for a description of magnitude determinations. STL Cerro Santa Lucia, Santiago, Chile. TAC National University of Mexico, Tacubaya, Mexico. See Lee and Wetmiller (1978) for a description of magnitude d.terminations. UPP Seismological Institute, Uppsala, Sweden. See Bath (1967) for a description of magnitude determinations. WCA Woodward-Clyde & Associates, 1969, Seismicity and Seismic Geology of Northwestern Venezuela, A report to the Shell Company of Venezuela, v. I and v. II.
I i7/ TABLE 6--MAGNITUDE SCALE CODE B Body-wave magnitude (for a description of the magnitude calculation, see references In table 5 for the source listed). E Estimated Ma magnitude based on macroseismic data. (chile, see text, p. 11.) G Local magni!, de. (Bolivia, see text, p. 10.) Magnitude determined from MSK-intensity data. (Peru, see text, p. 12.) K Magnitude converted from MSK--intensity data using Gutenberg and Richter's (1956) formula. (Ecuador, see text, p. 12.) M Pody-4ave magnitude converted from MM-intensity data. (Bolivia, see text, p. 11.) p Body-wave magnitude converted from PAS magnitude (Bolivia, see text, p. 10). S Su fane-wave magnitude (for a dccription of the magnitude calculation, see references In taLle 5 for the source listed). W Moment magnitude (from Kanamori, 1977).
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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.
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INTRODUCCION I. Investigadores clab
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7. Io t ermi i (i ojliiao s i dad !
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INTRODUCC1ON 47 CA'ALOOI ) I)t.E TF
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4Q) ciertos recientes evento:s gi a
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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
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59 I so ejemplifican algunos tomado
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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
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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
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77 Colombia y en la Cuenca d la Ama
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'FAiLA 5 - tCHDI T ,IA W FUENK:TES
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TAG Uniiye rsia IN(( N;wci on.i (.'
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83 TABLA 7 - INTtERPRETES APO Oscar
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711 No not nd. ,.a(~ i n V-npz;o Ia
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x / TABA F.- K Fi! N(:IAS 101 Infor
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31i3 lescotes, P.M., and Cahr,', Gc
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422 Polo, J.T., 1904, Sinopsis do t
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P.114411 > .iII, 11.Ci'144 1 P . ,
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9 5 REFI EN(CI AS CITADAS Bath, M.,
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Introducti on 97 SOUTH AMERICAN HYP
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99' Country Coordinator Investigato
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101 is provided for four, magnitude
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S03 These bulletins, for the time s
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locally which actually fell in Colc
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Brazil: Magn!tudes (mb) were comput
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intensities but also the distributi
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assigned the iJntonnsity value is a
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Shallow: 0-70 kms. S11 Intermediate
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115 compiled, is to more clearly de
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INTRODUCTION 117 CATALOG OF EARTHQU
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I 9 The criteria for tbe selection
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121 Mendoza: Vil].a Atucl and las t
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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
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: t 75 TABLE 5--Continued JGG Grases,
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
Page 191 and 192: 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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