Ab. Akopova et al., USE OF NUCLEAR PHOTOEMULSIONS TO INVESTIGATE THE SPITAK EARTHQUAKE AFTERSHOCKS, Nuclear tracks & radiation measurements, 21(3), 1993, pp. 317-321
The radon and thoron emanation in soil gases in the epicentral zone of
the Spitak earthquake of 7 December 1988 was estimated by the use of
nuclear photoemulsions. For measurements of the emanation flow, the st
ationary observation points of the Laboratory of Seismogeochemistry of
the Institute of Geological Sciences were chosen. The maximum flow wa
s detected in the observation point near the village of Saralandzh. He
re, the obtained value exceeded by 10.1 times the average level in the
Spitak region (the observation point in the town of Spitak). The flow
in the north-west wing of the Spitak break was considerably less and
exceeded the average value by only 2.1 and 1.5 times (Gegasar and Nalb
and villages). A comparative analysis of our data with those obtained
in the same observation points by means of the atmogeochemical method
shows rather good agreement between the experimental results. The join
t application of these two methods allows representation of the geodyn
amics of the region and prediction of earthquakes.