Exact(8)
Implementation of this technique on the sinogram is shown in Figure 11. Figure 11 Correction of Type 1 faults.
When D/S is larger than 1, faults are totally breached, or at the "hard-linkage" stage.
(1) Faults formed whilst the sediments are unconsolidated show evidence of sands being sheared down the fault plane forming disaggregation bands parallel to the fault plane.
When D/S is between 0.27 and 1, faults are at a stage of fault initiation, also at the "soft-linkage" stage.
During stage 1, faults initiate by shear along pre-existing structures (formed during an earlier event), or by the initiation of precursor structures (formed earlier in the same deformation event).
All stripes of the artifact corresponding to Type 1 faults are replaced with a constant value higher than the maximum value of the sinogram so that these stripes can be identified by the algorithm as the target region.
Similar(52)
1) Fault location .
Figure 1 Fault geometry.
Figure 1 Fault-detection system.
Then, after every 200 steps, the operating mode was changed in such a scheme: normal, fault 1, fault 2, fault 3, fault 4, fault 3, fault 2, fault 1, and normal.
Fault conditions are as follows: 1) Fault type: Single line-to-ground faults of phase B. 2) Fault resistance: 1 Ω. 3) Fault location: 50% of line 2. .
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