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 |
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 |
l |
Several
running averages are computed
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|
|
for this
sequence in the trailing time
|
|
|
window (t - s,
t) and magnitude range
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|
M0 > Mi
³ m.
|
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|
l |
They depict
different measures of
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|
|
intensity in
earthquake flow, its deviation
|
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|
from the
long-term trend, and clustering of
|
|
earthquakes.
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|
The
averages include:
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|