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Intermediate-term earthquake prediction
Pages 3748-3755

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From page 3748...
... It was found that the approach of a "strong" earthquake may be indicated by certain patterns in an earthquake sequence; they are called premonitory seismicity patterns and are used in prediction algorithms reviewed here. A test of prediction algorithms is crucially important, since they are inevitably adjusted retrospectively.
From page 3749...
... In robust definition, the normalized premonitory phenomena are identical in the magnitude range of at least M - 4.5 and for a wide variety of neotectonic environments (12-14) , which include subduction zones, transform faults, intraplate faults in the platforms, induced seismicity near artificial lakes, and rock bursts in mines.
From page 3750...
... Star shows the epicenter of the Loma Prieta earthquake. Solid polygon shows the reduced area of alarm; it is determined in retrospection by applying algorithm Mendocino Scenario described below.
From page 3751...
... We see that prediction by algorithm CN is more reliable for strong earthquakes, which occur on an average once in 7-10 years (N = 0.15-0.1~; prediction of stronger earthquakes should probably be made separately, in larger areas. This breakdown is not made for the retrospective test, since the magnitudes were often rounded up to 0.5 during the corresponding time intervals.
From page 3752...
... Circles and dark polygons show alarm areas obtained respectively by MS and Mendocino scenario algorithms. Small open circles show actual epicenters of strong earthquakes.
From page 3753...
... Of particular promise is an analysis of precursors with time measured in the number of the earthquakes within a certain magnitude range (51~. This time scale allows one to make a uniform analysis of foreshocks, main shocks, and aftershocks.
From page 3754...
... . Nevertheless, in earthquake prediction research long-range correlations are often regarded as counterintuitive, probably on the ground that in a wide class of simple elastic models redistribution of stress and strain after an earthquake would be confined to the vicinity of its source (Saint Venant principle)
From page 3755...
... (1982) in Earthquake Prediction Research, ed.


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