2022
DOI: 10.1016/j.coal.2022.104044
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Maturation study of vitrinite in carbonaceous shales and coals: Insights from hydrous pyrolysis

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Cited by 12 publications
(2 citation statements)
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“…The significant reduction in HI values in higher pyrolysis temperatures may be related to the conversion of labile H-rich liptinitic organic components . The production index (PI = S 1 /(S 1 + S 2 )) is a thermal maturity proxy and PI > 0.10 is a remarker as the source rock entered the peak oil window . The original PI values for shale 22-8 and 23-10 and mudstone 37-5 and 27-8 are 0.09, 0.07, 0.05, and 0.12, respectively (Figure b), indicating samples under the immature to mature stage .…”
Section: Resultsmentioning
confidence: 99%
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“…The significant reduction in HI values in higher pyrolysis temperatures may be related to the conversion of labile H-rich liptinitic organic components . The production index (PI = S 1 /(S 1 + S 2 )) is a thermal maturity proxy and PI > 0.10 is a remarker as the source rock entered the peak oil window . The original PI values for shale 22-8 and 23-10 and mudstone 37-5 and 27-8 are 0.09, 0.07, 0.05, and 0.12, respectively (Figure b), indicating samples under the immature to mature stage .…”
Section: Resultsmentioning
confidence: 99%
“…48 The production index (PI = S 1 /(S 1 + S 2 )) is a thermal maturity proxy and PI > 0.10 is a remarker as the source rock entered the peak oil window. 49 The original PI values for shale 22-8 and 23-10 and mudstone 37-5 and 27-8 are 0.09, 0.07, 0.05, and 0.12, respectively (Figure 5b), indicating samples under the immature to mature stage. 50 After 345 °C, the PI of pyrolyzed samples increased dramatically; this indicates that the samples entered the main oil generation stage (Figure 5b).…”
Section: Rock-eval Pyrolysismentioning
confidence: 99%