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The optimum angle at which EEI log and the target petrophysical parameter give the maximum correlation was meticulously analyzed by additionally incorporating the concept of relative rock physics.
The maximum correlation was of early score EBV1 3 on SCORE1 9 at 4+ years old (r = 0.22).
The LARS iterations were carried forward until the maximum correlation was reached.
The subset sizes considered ranged from 1 to 8, with a full enumeration from 1 to 3 and a stepwise procedure from 4 to 8. Similarly, the PRK variables were first computed on the first bootstrap sample and the RK stage with the maximum correlation was chosen.
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It is evident that maximum correlation is obtained at.
It is apparent that maximum correlation is obtained at (Figure 2) for this range of angles.
Maximum correlation is attained when a spatial cluster is located around.
The IMF reporting maximum correlation is chosen and NASE is again calculated.
Based on fundamental properties of this transform, maximum correlation is identified with a line structure in the time frequency plane.
The global maximum correlation is obtained for α=1 and β=0.7 for both, 8 and 4 multi-sequences.
After all candidate rotation angles and scaling factors have been searched in this way, the orientation and scale corresponding to the maximum correlation are adopted as the estimated parameters for rotation and scaling.
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