14.12.2012 Views

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

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

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

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

100<br />

in any way checkea or edited. Areas covered by each country do not overlap,<br />

so that when these <strong>catalog</strong>s are combined <strong>earthquakes</strong> should appear in the<br />

<strong>catalog</strong> only once.<br />

The <strong>catalog</strong>s cover a time period beginning with the earliest known<br />

historical events and ending with Deceber 1981. The earliest event inclu<strong>de</strong>d<br />

occurred in 1471. The completeness <strong>of</strong> tha <strong>catalog</strong> varies over Eime, bnlng<br />

relatively ncomopl.ce for early historical events and much more complete for<br />

recent. ,venitu . The lower magnitudo cut<strong>of</strong>f has been <strong>de</strong>signated as 4.5 mb<br />

,<br />

Smaller events have not been vigorously eHiminated, particularly since many<br />

events have no reported or calculated magnitu<strong>de</strong>. The <strong>catalog</strong>, however, is<br />

much less complete for events below magnitudc 4.5 mb.<br />

A <strong>de</strong>scription <strong>of</strong> the hypocenter <strong>catalog</strong> format is listed in Appendix A.<br />

Tables -3 cocrib codrs used in the format, Including references for the<br />

sources ised. The two-letter country uo<strong>de</strong> l;ogether with the five-digit<br />

i<strong>de</strong>ntif.-ing number (columns 2-9) provi<strong>de</strong> a unique reference for each event.<br />

The errors associated with quality factor co<strong>de</strong>s for time, epicenter, and <strong>de</strong>pth<br />

are <strong>de</strong>scribed in 7'bles 1, 2, and 3, respectively. Quality factors used by<br />

other sources for hypocenter data, were converted to the factors <strong>de</strong>fined for<br />

this <strong>catalog</strong> as indicated in Tables 1, 2, and 3. These relationships were<br />

<strong>de</strong>terminecd hy L. Ocola in the early phanns <strong>of</strong> the <strong>catalog</strong> project. The co<strong>de</strong> X<br />

is used in all three tables when the quality is unknown or un<strong>de</strong>fined. In many<br />

cases, a good estimate <strong>of</strong> the error for the hypocenb,.. is not available, but<br />

knowing whether tt is instrumentally <strong>de</strong>termined or <strong>de</strong>rived from macroselsmic<br />

data gies some vadditinal information about the probable error. Therefore,<br />

the co<strong>de</strong>s M for macroseismic and I for instrumental have been used in place <strong>of</strong><br />

X for epicente; and <strong>de</strong>ptlh quality factors if this information is known. Space

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!