Exact(1)
However, the recurrence interval of such an eruption is approximately 15 to 20 thousand years (Dominey-Howes and Minos-Minopoulos, 2004) and the consensus interpretation is that Santorini is in a post-caldera shield-building stage of volcanism.
Similar(59)
Hence, the intervals are called confidence intervals; the end points of such an interval are called upper and lower confidence limits.
In fact, if ϕ vanishes on an interval, then ϕ ′ = 0 at the boundary of such an interval where ϕ > 0 or ϕ < 0, which contradicts the maximum principle.
Then the formula for calculating the interval violation vector of such a constraint should be adjusted as Eq. (4).
In this case, the constraint (g_{i} left( {{varvec{x}},{varvec{U}}} right) le B_{i} = [b_{i}^{L},b_{i}^{R} ]) in Eq. (1) degenerates as (g_{i} left( {{varvec{x}},{varvec{U}}} right) le b_{i}) and the formula for calculating the interval violation vector of such a constraint should be adjusted as Eq. (5).
This interval represents the most bursty and congested interval for a given application and so the allocation of one more resource instance to the bottleneck tier of such an interval is likely to result in the most reduction in the application's V a when compared to other intervals.
The Bayesian interpretation of such an interval is "there is a 95% probability that the true percentile rank of the patient's score lies within the stated interval".
Recurrence interval of such giant earthquake ranges from 400 to 740 years.
Giving the plate convergence speed of 8.3 cm/yr, the recurrence interval of such kind of events would be much longer than 500 yr.
Like other active faults with low slip rate, the recurrence interval of such large earthquakes along the Crocker fault system is likely to be in the order of several thousand years.
The averaged seismic coupling of 0.5 0.8 in the M 9 earthquake's source area and the seismic moment of the earthquake suggest that the slip deficit for the M 9 earthquake was accumulated over a period of 260 880 years, consistent with the recurrence interval of such great earthquakes from tsunami deposit data.
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