Sentence examples for conventional reflection from inspiring English sources

All the data were processed using techniques employed in conventional reflection surveys.

The conventional reflection section provides higher quality image of the crust compared to the wide-angle section.

Conventional reflection seismics usually fails to produce a satisfactory image of the pre-Permian strata due to the shielding effect of Zechstein (Upper Permian) evaporites.

However, the conventional reflection and refraction laws may be violated in the presence of a metasurface, and reflection and refraction at the metasurface obey generalized laws of reflection and refraction (Yu et al., 2011).

It allows us to perform conventional reflection and transmission measurements including rocking curve measurement as well as polarimetric and ellipsometric measurements based on the rotating-analyzer method by using six independently movable motorized stages.

This has been measured using a novel variant of the traditional sin2 ψ method using low scattering angles in transmission rather than backscattering in the conventional reflection geometry that exploits the high penetration of high energy synchrotron X-rays.

Conventional reflection-type SPR biosensors, employing a prism, however, also present several drawbacks and usually lack the sensitivity to detect the interaction of proteins with small ligands [11].

The conventional seismic reflection processing methods for detecting and suppressing multiples tend to fail in some circumstances.

This enables to easily localize mica flakes and rapidly estimate their thickness directly on gold substrates by conventional optical reflection microscopy.

A rectangle with red broken line marks the area expanded in Fig. 10 Fig. 10 Enlarged composite profile of conventional seismic reflection and attenuation profiles without fault interpretation (a) and with fault interpretation (b).

Faults were imaged as high-attenuation stripes, demonstrating that SAP may contribute to detection of faults in the igneous section of oceanic crust where faults are rarely imaged by conventional seismic reflection methods.