Sentence examples for mapping of shallow from inspiring English sources

The HVSR (Horizontal to Vertical Spectral Ratio) technique is very popular in the context of seismic microzonation and for the mapping of shallow seismic reflectors, such as the sediment/bedrock transition surface.

Given the lengthy perimeter of coastlines, there is a need for cost-efficient methods for producing high resolution maps of shallow areas.

However, there appears to be a dynamic sulfur cycle at the site, featuring both biotic and abiotic sulfur oxidation and reduction [67],[68],[70]–[72]. Figure 1 Map of shallow sea hydrothermal vents.

These values were chosen to enable optimal mapping of both shallow and deeply seated structures (>100 m), assuming that penetration is about 1/6 of maximum current electrode spacing.

Mathematical construction of a sub-surface model from the local anomaly data, employing a 3D inversion based on "growing" the sub-surface density distribution via the aggregation of cells, enables mapping of the shallow structure beneath the complex, giving unprecedented insights into the sub-surface architecture.

To identify single-copy sequences, multiple genome equivalents of short SOLiD reads of another individual were mapped to shallow genome coverage of long Sanger or Roche 454 reads making up the reference sequence.

Open image in new window Fig. 8 Isopach maps of the shallow (a) and main (b) aquifers.

Open image in new window Fig. 7 Isobath maps of the shallow (a) and main (b) aquifers.

The isopach maps of the shallow (Fig. 8a) and main aquifers (Fig. 8b), compared to the isobath maps show the same traits.

Fig. 2. (a) Epicenter map of the shallow earthquakes (MJ = 4.0 and depth = 100, 1 January 1926 to 22 September 2003) from the JMA catalog; (b) a space-time plot of latitudes against occurrence times, and (c) a space-time plot of occurrence times against longitudes.

In AGSNP, deep genome coverage of NGS reads from one homozygous individual was mapped to shallow 454 reads of another homozygous individual.