 |
|
|
|
|
|
|
|
|
|
Qualitatively,
the MSc algorithm outlines such an
|
|
|
area of the
territory of alarm where the activity,
|
|
|
from the
beginning of seismic inverse cascade
|
|
|
recognized by
algorithm M8 in declaration of the
|
|
|
alarm, is
continuously high but infrequently
|
|
|
interrupted
for a short time. Such an interruption
|
|
|
must have a
sufficient temporal and/or spatial
|
|
|
span. The
phenomenon, which is used in the MSc
|
|
algorithm,
might reflect the second (possibly,
|
|
|
shorter-term
and, definitely, narrow-range) stage
|
|
|
of the
premonitory rise of seismic activity near
|
|
|
the incipient source of
main shock.
|
|