Exact(2)
The color of conventional chemical synthesized silver nanowire solution is pale green accompanied with strong reflection [4] due to the narrow resonance bands and selective light localization properties.
The deep mega-splay fault landward of the transition zone off Kumano has been imaged as a single reflector with strong reflection amplitude (Figure 2; Park et al. 2002; Bangs et al. 2009), indicating a large contrast in seismic velocity (Tsuji et al. 2006; Kamei et al. 2012), which in turn originates from large pore pressure contrast or difference in lithology.
Similar(58)
The amount of the received signal refers to a color gradient, where bright colors denote areas with strong reflections (mainly due to significant changes in density between structures like elastin, connective tissue, and collagen) and dark colors refer to areas with low reflection (ie, little or no change in density of structures present in the skin, such as fluid, fat, and blood).
And with such a strong reflection in the lake and much to reflect upon it, it is a great place to capture abstract photographs.
The seismic data quality is good to excellent with numerous strong reflections in raw shot gathers, resulting from a careful survey design that included test shots and a priori considerations for the geological environment.
Therefore, the superhard coatings with a hardness of H>40 GPa are characterized either by the strong reflection from large (20 50 nm) ZrNx grains with a preferential orientation or by many weak reflections from small, approximately 10 nm, ZrNx grains.
Additionally, the samples from the organic experimental group appear a strong reflection in their red-spectrum area, which agrees with the samples' overall optical appearance of being reddish.
An agar phantom was used as a bottom layer to prevent an overlap of strong reflection signals from the bottom of the case with backscattered signals from the thrombus.
In most cases the boundary was successfully detected because of the strong reflection at the boundary, however the boundary in regions with low SNR or regionally saturated OCT data were not accurately detected.
SHARAD has provided strong evidence that the LDAs in Hellas Planitia are glaciers that are covered with a thin layer of debris (i.e. rocks and dust); a strong reflection from the top and base of LDAs was observed, suggesting that pure water ice makes up the bulk of the formation (between the two reflections).
While some bolt-plates provided a strong reflection and hence maximum signal amplitude, in other cases the contrast with the background coal was not sufficient to allow discrimination.
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