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Geochemical divergence of oxygen and sulfur compounds in high-maturity bitumen: Implications for thermal maturity assessment
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DOI:10.1016/j.apgeochem.2026.106965.png)
Abstract
En 中文
• O2 compound trends reverse at high maturity: complex molecules crack into simpler products. • S1 compounds show maturity-invariant DBE via dynamic equilibrium, limiting utility. • Novel maturity parameters based on FT-ICR MS correlate well with GC-MS indices.
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3.4
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5.9K
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