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The conventional reflection section provides higher quality image of the crust compared to the wide-angle section.
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).
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.
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Also, we have found that the calculated spin polarization can be used as a tool to distinguish specular Andreev reflection (SAR ) from the conventional Andreev reflection (CAR ) such that in the case of CAR, spin polarization in sub-gap region is completely negative which means that spin-down current is greater than spin-up current.
For comparison purposes, Fig. 4 d) also illustrates the results of a conventional reflection mode bench-top microscope imaging the same specimen taken with a 4X objective lens (0.1 NA), which agrees well with our field-portable lensfree reflection microscope results.
This approach allowed a free flow of ideas and discussion, without the boundaries of an interview and conventional reflection.
The conventional seismic reflection processing methods for detecting and suppressing multiples tend to fail in some circumstances.
All the data were processed using techniques employed in conventional reflection surveys.
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.
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.
For conventional reflection survey data processing, velocity information is observed using NMO correction and CDP stacking; it cannot address lateral variations of the structure because the algorithm defines the subsurface structure as a flat multilayered structure (e.g., Al-Yahya 1989; Stork and Clayton 1992).
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