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The thickness of the unit ranges from 10 cm to 50 cm.
The thickness of the unit ranges from 10 to 30 cm.
The thickness of the unit cell structure of clay mineral is relatively small but when moisture water is absorbed into this structure, its thickness increases.
The sharp spectral contrast between bluish Unit E and the other reddish older units (Fig. 2c) allows us to infer the thickness of the unit by using the small craters that penetrate through Unit E. The depth of a simple crater is about 1 / 5 of its diameter (e.g., Pike 1977).
The nanolaminate-Al2O3/TiO2 sealing layers were obtained by repeated sub-cycles of Al2O3 and TiO2, respectively, as mentioned above, whereas the thickness of the unit cycles was fixed at ~2 nm for both, and the number of deposition cycles for each of the unit cycles was calculated using a growth rate per cycle (GPC) of ~1.5 Å/cycle for Al2O3 and ~0.3 Å/cycle for TiO2.
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The thickness of this unit in the LOC ranges between 143 and 149 km, and its composition is modeled from the database reported in McDonough (1990) and the update in Huang et al. (2013).
Two material designs were compared: one in which the densities of the materials used for the unit plate panel and the grid were changed relative to each other, and a second where the relative thicknesses of the unit plate panel and the grid frame were varied.
For example, if a 500-m-diameter crater penetrates through the uppermost unit and reaches to the underlying unit, the thickness of the uppermost unit at the point is estimated to be thinner than (sim 100 m.
Factors that showed the most significant correlation with the total depth of undercutting were found to be the vertical distance of the undercut unit from the slope crest, the relative position of the undercut unit from the slope crest, the total thickness of the undercut unit, joint spacing within the undercut unit, and the slake durability index of the undercutting unit.
The density of the Quaternary sediments (Q) was fixed at 1.9 g/cm3 because the thickness of this unit is less than 100 m such a thin geologic layer is difficult to resolve considering the wide spacing of the gravity stations.
The thickness of this unit at Soultz-sous Forêts is therefore thinner than it is regionally.
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