D. Colombo et al., APPLICATION OF PATTERN-RECOGNITION TECHNIQUES TO LONG-TERM EARTHQUAKEPREDICTION IN CENTRAL COSTA-RICA, Engineering geology, 48(1-2), 1997, pp. 7-18
The expert system GEO 2.5 has been applied to the analysis of geophysi
cal and geological data from Costa Pica. Geophysical data consist of s
eismic tomography, Bouguer anomalies, seismic catalogue (RSN-ICE, 1984
-1993) and seismic historical catalogue. Among the geological data, fa
ults, lineaments, topography and a structural zonation of the region c
oncerned have been used. Many other features have been obtained throug
h the calculation of statistical functions of the original data such a
s nearness, density, length and b-value, other functions were secondar
y derivatives and modulus of horizontal gradient. A first analysis, ma
inly based on seismic tomography data and seismic catalogue, has led t
o the identification of a few seismogenic structures in the upper crus
t characterized by a high statistical correlation coefficient between
seismic activity and positive velocity anomalies. Pattern recognition
techniques have been applied to the long-term earthquake prediction by
the definition, in the feature space, of non-linear regression functi
ons between geophysical/geological data and a preliminary estimate of
expected maximum magnitude. This preliminary estimate has been formula
ted on the basis of both the historical seismic catalogue and the stru
ctural zonation. This approach gives the empirical relationships among
different geophysical and geological features, which are potentially
related to the phenomenon of stress release. Due to the high non-uniqu
eness of such an approach, the results have to be physically understan
dable and each function has to be interpreted. The obtained multi-dime
nsional function has been applied to the calculation of a forecast max
imum magnitude field for central Costa Pica. The results are to be con
sidered preliminary. An improvement of such a forecast could be achiev
ed by new data, such as heat flow, depth of Mohorovicic surface, activ
e faults, vertical movement velocities, etc. (C) 1997 Elsevier Science
B.V.