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By changing the sight angle of the high-resolution bathymetric maps, we determined the strike of the linear fault scarplet (yellow arrow in Figure 5b) and the sense of dip slip along it; the clearest fault trace located on the trenchward side of the pull-apart basin is downthrown on the north.
Besides calculation of CBV maps, we determined the intensity time curve within the ROI with the highest rrCBV value.
In the remaining 5 maps we determined the location of the imaging site relative to the barrel using alignment of vertical blood vessels.
Using single-molecule maps that partially aligned to EBV reference maps and partially to the hg38 reference maps, we determined the EBV integration sites in all three samples.
To quantitatively analyze the connectivity maps, we determined (1) the density and (2) the strength of synaptic inputs arising from a given layer.
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Based on the mapping, we determined that V3 sequence variation accounted for neutralization resistance of approximately half the viruses tested.
To further analyze the quality of learners' interaction with MIC-O-MAP, we determined the productive value action (PVA).
By high-resolution genetic mapping, we determined that st67 disrupts the zebrafish homolog of sec63.
Using the values of the concentration map, we determined that most of the CaM molecules are part of molecular complexes.
For CIM on the consensus map, we determined the simple interval mapping LOD thresholds through 1000 permutations with a genome-wide error rate of 5%.
Using a statistically obtained, high-confidence, stable nucleosome map, we determined the exact distance between the dyad of the +1 nucleosome and the TSS for all genes.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com