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The oil-prone nature is revealed by the cross plot between vitrinite reflectance and hydrogen index.
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It is difficult to obtain rock resistivity parameters by using the cross plots of porosity vs. formation factor and water saturation vs. resistivity index to calculate reservoir water saturation in low permeability sandstones.
The cross-plot of Vp versus Rho as modified by Swarbrick (2012) was used to check for secondary mechanism and complimentary to Lahann et al. (2001) plot.
The lithology correction was done using the cross-plot.
No obvious nonlinear relationship emerged from the cross-plots.
Provenance, i.e. the geographical site of residence, can be revealed individually or by a cross plot of the elemental ratios Sr/Ca and Ba/Ca [18, 50].
This lignite falls closer to the zone of organic rich type-III kerogen which is formed under topogenous condition as also revealed by a cross plot between total organic carbon (TOC) and sulfur content (Fig. 7).
We obtained the parameters by drawing cross plots between the λ and effective coefficient of basal friction μ b ′ (Figure 4) by referring to Wang et al. ([2010]).
The crack-tip opening angle (CTOA) was firstly determined by the cross-sectional plots.
Three wells in the target area were used to constrain the inversion results by cross plotting ln AI versus ln GI in one hand, and ln AI versus ln Vp in the other hand.
We assumed that the clay volume primarily consisted simply of illite and the rest clay minerals and figure out the volume of illite by using neutron-density cross plot.
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