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Fig. 8 Plot of core analysis data from a local field.
Open image in new window Fig. 6 Plot of core permeability versus predicted permeability for field W-continental/fluvial environment .
Open image in new window Fig. 7 Plot of core permeability versus R tot predicted permeability for Field W-continental/fluvial environment.
Open image in new window Fig. 10 Plot of core permeability versus R tot predicted permeability for field Z- tidal/estuarine environment.
Open image in new window Fig. 8 Plot of core permeability versus R tot predicted permeability for field X-turbiditic/DW environment.
Open image in new window Fig. 9 Plot of core permeability versus R tot predicted permeability for field Y-coastal/distributary environment.
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a Shell-derived δ 18Osw and calcification salinity plot of core-top samples in this study and the literature.
Fig. 5 Latitude-azimuthal-speed power plot of the core surface radial component of the sub-centennial constituent.
Track 5 of Fig. 5 presents a plot of corrected core permeabilities with reference to the predicted from the proposed (overline{{R_{{{text{tot}} }} }}), SDR and Coates models.
The Te value of the full model as each altitude and season, Te(mlt, invdip, PF10.7), is obtained by addition of the core model value Te0(mlt, invdip) and of the solar activity term TePF10.7(mlt, invdip, PF10.7): (6). Figure 4 shows the contour plot of the core model for all five altitudes and both seasons (equinox and solstice).
b Ba/Ca G. ruber ratios and calcification salinity plot of all core-top samples in this study.
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