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Various sand bodies have been identified by these reflection patterns.
Flower-structure-like reflection patterns (around CDP 23,500 24,000).
Figure 7b shows the electron reflection patterns relative to the first and the 30th final bilayers.
The net results of their effects are to disrupt coherent Lg reflection patterns in the crustal waveguide.
The weathered layer exhibits nearly smooth to smooth reflection patterns with a thickness range of about 7.0 17.4 m.
Therefore, because the reflection patterns are diffuse, they can correctly be approximated using the Lambertian reflection model.
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It is the contrast in the dielectric permittivity between the subsoil that causes reflections: the greater the difference in dielectric permittivity (variation in textural, lithology and porosity of subsoil), the greater the coefficient of reflectivity [7] which translates GPR reflection pattern variations.
UV-vis diffuse reflectance spectroscopy (DRS) was carried out in diffuse reflection pattern with a spectrophotometer (Lambda 950, Perkin Elmer) equipped with a wavelength range of 200 800 nm (BaSO4 as a reference).
where RS is the model used to describe the reflection pattern.
This unit (U3b) consists of a semitransparent, chaotic reflection pattern suggesting mass transport deposition (MTD).
All volcaniclastic units reveal the same transparent reflection pattern strongly suggesting that explosive underwater volcanism was the prevalent process.
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