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Note that no M 7 earthquake occurs in the region above the shallow segment (depth: 60– 80 km) because of its shorter length.
(2) The second M 7 earthquake (M=7.1 7.7) occurs in a midst segment (depth: 110 140 km) of seismic regions in the middle of each century (37 45 years).
(3) The third M 7 earthquake (M = 7.1 7.5) occurs in a shallow segment (depth: 80 110 km) of seismic regions at the end of each century (77 94 years).
(1) The first M 7 earthquake (M = 7.1 7.9) occurs in a deep segment (depth: 140 160 km) of seismic regions at the beginning of each century (1 16 years).
From the hypocenter relocation image obtained by Hurukawa et al. (2008) and the observed periodicities of earthquakes in the seismic regime, it is highly probable that the next strong shock will be generated by around 2010 in the deep segment (depth: 140 160 km) of the Vrancea focal volume.
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Yet, while low resolution of the ToF camera is enough to segment depth-based areas, higher-resolution RGB camera allows for accurate image processing.
For optimization and determination of the model parameters [i.e., the segment diameter, depth of pair potential (ε/k), and the average of the pure species segment number (m)], history matching was used.
Open image in new window Fig. 4 a Shape of the CRS operator corresponding to a curved reflector segment in depth; b shape of the CDS operators corresponding to the same diffraction point, [a from Heilmann (2007) and b from Soleimani et al. (2009b)].
Soil cores taken to depths beyond the solum, were segmented with depth, and total SOC was determined for each segment on an equivalent mass basis.
The length of these collagen segments is depth dependent with short (≤5 µm) anterior and long, regularly spaced posterior segments (as long as 50 µm in swollen corneas).
Furthermore, new coding tools (such as depth-modeling mode (DMM) and segment-wise depth coding (SDC)) are exploited for the characteristics of depth map to improve the coding efficiency.
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