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years 1966, 1967, 1968 and 1969 is investigated. This earthquake activity
as a rule follows the general pattern found by the use of data for a much
longer period. There is a clear tendency for the focal depth of the earthquakes
to increase from the convex side of the Aegean arc to the inner volcanic
The value of the constant b of the recurrence curves is much smaller
for the intermediate earthquakes than for the shallow ones.
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