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AAPG Bulletin
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AAPG Bulletin; Year: 2024; Issue: February DOI: 10.1306/12202222033
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Figure 6.
(A) Relative thickness of siliciclastic mudstones (i.e., organic-rich siliceous mudstone and argillaceous mudstone) and carbonates in the studied Wolfcamp interval. (B) Median nuclear magnetic resonance (NMR) porosity (black area) and helium porosity (gray area) in tested samples from siliciclastic mudstones (n = 17 samples) and carbonates (n = 23 samples) lithofacies. The thickness of the bars is proportional to the relative thickness of each lithofacies according to (A).

Figure 6. (A) Relative thickness of siliciclastic mudstones (i.e., organic-rich siliceous mudstone and argillaceous mudstone) and carbonates in the studied Wolfcamp interval. (B) Median nuclear magnetic resonance (NMR) porosity (black area) and helium porosity (gray area) in tested samples from siliciclastic mudstones (n = 17 samples) and carbonates (n = 23 samples) lithofacies. The thickness of the bars is proportional to the relative thickness of each lithofacies according to (A).