3b ), leading to an increasing trend of C 1 /ΣC 1–5 ratio (Fig. 3f ).
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Isothermal confined pyrolysis on source rock and kerogens in the presence and absence of water: Implication in isotopic rollover in shale gases.
1
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3b ), leading to an increasing trend of C 1 /ΣC 1–5 ratio (Fig. 3f ).