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Many wackes contain much mud, typically 15 40 percent, and this increases as the mean grain size of the rock decreases.
Figure 1 Evolution as a function of mean grain size.
NSP: net sandstone percentage; MGS: mean grain size.
The results showed that the sensitivity of Gmax to pressure increased with decreasing mean grain size.
Additionally, the mean grain size is reduced to about 13 nm.
Surprisingly, it was evidenced that there is unequivocal link between mean grain size with dielectric properties.
In Figure 3, the coercive field is showed as a function of the mean grain size.
When the thickness of the samples is increased, the crystallinity and the mean grain size improved.
Similar(3)
The mean grain-size probability densities for and 1500 OH/10Si are very similar.
We interpret the mean grain-size field in terms of its permeability to melt transport.
Figures 4i and 4j show the resulting mean grain-size field.
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