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The underground structure models identified by Satoh et al. (2001a) are set as the initial models with a priori information, and the underground structure is inverted using the inversion method described above.
These chromosome-specific models were then subsequently used as the initial models (M) for the LRT analysis described above.
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These final modes were internally validated by bootstrapping as for the initial models.
These estimates were used in this study as the initial model for the 3-D inversion.
This map was used as the initial model for subsequent image processing.
Then, the best model was used as the initial model, and as the prior model for the series of iterations in the next generation.
Also for the cause of merging models, the "medoid" model in a cluster has been selected as the initial model.
Also for the cause of merging models, the medoid model in a cluster may be selected as the initial model.
Secondly, we choose the simplified structure as the initial model and then invert the structure using the stochastic inversion technique.
The tomographic inversion results showed almost the same structure as the initial model, but with smaller structural perturbations (Fig. 7).
A crystal structure of the 30S subunit (PDB ID: 3OFA) (Dunkle et al., 2010) was used as the initial model.
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