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Concerns have been raised about the reproducibility of dipping data based on one 24-h period [ 46, 56– 58].
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The BHTV shows a fracture oriented N-S and dipping westward (data from DMT-Institute for Geophysics, Germany).
The BHTV shows a conjugate fracture system with a major structure dipping westward (data from GEIE EMC, France). Figure 11 Equilibrium temperature profile from 0- to 1,500-m 1,500-mn the well 4550.
The investigation of complex geological setting is still dominated by traditional geo-data collection and analytical techniques, e.g., stratigraphic logging, dip data measurements, structural ground mapping, seismic interpretation, balance section restoration, forward modelling, etc.
While the model has since been updated (see http://on.doi.gov/h32IYb; Fig. 2(d)) to better account for subduction zone dip, data distribution and quality, the general along-strike and up-dip distribution of slip estimated by this first model is very similar to those shown in a variety of models released since that time.
Taking MCODE on DIP data as an example, it has predicted 50 complexes, of which 44 match 21 real complexes.
In Figure 4, we observe that MCODE was able to achieve the highest precision in DIP data.
Tables 1 and 2 show the detailed comparative results of the various computational detection methods on the DIP data and the Krogan data, respectively.
We have compared these techniques over two publicly available benchmark yeast PPI datasets, namely DIP data [ 93] and Krogan data [ 33].
For instance, the inflation parameter in MCL was set as 1.9 on DIP data [ 37] and the minimum cluster size of RRW was set to 5 [ 16].
(15) S n = ∑ i m a x j T i, j ∑ i | b i |, P P V = ∑ j m a x j T i, j ∑ j | ∪ (b i ∩ p j ) |, A c c u r a c y = S n * P P V We compared the performance of PLW with 11 state-of-the-art methods on DIP data.
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