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

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intensities but also the distribution <strong>of</strong> observed intensities in converting MM<br />

intensities to MSK intensities.<br />

Intensity DaLa<br />

A summary <strong>of</strong> the intensity <strong>catalog</strong> format is given in Appendix B.<br />

Detailed intensity data are given for some <strong>of</strong> the events inclu<strong>de</strong>d In the.<br />

hypocenter <strong>catalog</strong>. Descriptive data provi<strong>de</strong>d by Silgado (1985) were not<br />

available at the time <strong>of</strong> the ccmpilation <strong>of</strong> the intensity <strong>catalog</strong> and, thus,<br />

may not be incluocd here. Two types <strong>of</strong> records, or line entriea, are inclu<strong>de</strong>d<br />

in the intensity <strong>catalog</strong>. The first is a single line for each event.<br />

<strong>de</strong>scribing the hypocenter <strong>para</strong>meters. Then for each event a number <strong>of</strong><br />

location records are Inclu<strong>de</strong>d which gives the intensity assigned for that<br />

earthquake at various locations. The intensity scale used (MM or MSK) is<br />

i<strong>de</strong>ntified for all listed intensities.<br />

The hypocentral i<strong>de</strong>ntification inclu<strong>de</strong>s much <strong>of</strong> the same information that<br />

is given for that event in the hypocenter <strong>catalog</strong>. The same country ca<strong>de</strong> and<br />

i<strong>de</strong>ntifying number are used in The intensily <strong>catalog</strong> as are used for that<br />

event in the hypocenter <strong>catalog</strong>. The date and time are also iisted the same<br />

but the time is only given to the nearest second in the intensity <strong>catalog</strong>.<br />

The intensity <strong>catalog</strong> allows space for two different epicenters; an<br />

instrumental epicenter and an epicenter <strong>de</strong>termined from intensity<br />

distribution. The reason for this is that the instrumental epicenter may not<br />

correspond very well with the center <strong>of</strong> the meizoseismal area. This may lead<br />

to additional uncertainty in the investigation <strong>of</strong> intensity attenuation.<br />

Therefore, in some instances it may be useful to inclu<strong>de</strong> both an instrumental<br />

epicenter and an epicenter based on the intensity distribution. Earthquake<br />

focal <strong>de</strong>pth is also given in the intensity <strong>catalog</strong> but to the nearest

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