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The mapping results are then weighted by using the multi-scale weighting algorithm.
Similar mapping results are obtained in one dimension, without excluding α∈(−1/2,1/2), by means of a local Calderón Zygmund theory and weighted Hardy's inequalities.
The results of the geomechanical analyses computed by PlaneDetect in comparison to the manual mapping results are more statistically reliable based on less user bias.
Therefore, only the interval mapping results are presented.
The mapping results are shown in Figures 8 and 9.
The mapping results are displayed as color-contoured images of the calculated water contents.
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The mapping results were validated using cross validation and an independent validation.
The characterizations of XRD, TEM, HRTEM, EDX, and local elemental mapping results were performed.
These elemental mapping results were strong proofs of the heterogeneous core/shell structure formation of the α-NaGdF4/β-NaYF4 Yb,Er crystals.
The FL-cDNA and FL-EST mapping results were clustered independently.
The mapping results were converted to pileup files with SAMtools [15].
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