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Home All issues Volume 73 (2018) Oil & Gas Science and Technology - Rev. IFP Energies nouvelles, 73 (2018) 49 Full HTML
Dynamics of sedimentary basins and underlying lithosphere at plate boundaries: The Eastern Mediterranean
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Table 7

Molecular geochemical ratios from GC-FID analysis. Pr = pristane; Ph = phytane; TAR = terrigeneous/aquatic ratio; OEP = Odd Even Predominance; CPI = Carbon preference Index.

Sample Age Pr/Ph Pr/n-C17 Ph/n-C18 TAR OEP CPI
15/892 Messinian 0.50 0.53 0.89 1.41 0.74 0.88
15/895 Eocene to Miocene 1.30 0.50 0.51 0.10 0.76 1.38
15/864 Bartonian to Priabonian 1.49 0.24 0.31 0.07 0.83 1.23
18/867 Bartonian to Priabonian 1.58 0.37 0.49 0.13 1.07 1.41
15/868 Bartonian to Priabonian 0.49 0.33 0.90 0.69 1.16 1.59
15/872 Bartonian to Priabonian 1.25 0.25 0.39 0.22 1.04 1.58
15/888 Ypresian to Lutetian 0.83 0.52 0.73 0.39 0.88 1.29
15/890 Ypresian to Lutetian 1.41 0.36 0.39 0.11 0.85 1.03
15/899 Turonian to Coniacian 1.48 0.54 0.49 0.56 1.11 1.13
15/902 Turonian to Coniacian 1.17 0.38 0.50 0.32 1.20 1.58
15/903 Turonian to Coniacian 1.00 0.31 0.41 0.20 0.99 1.29
15/906 Turonian to Coniacian 1.49 0.32 0.31 0.06 0.94 0.94

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