2015
DOI: 10.1016/j.coal.2014.12.006
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Geochemical and petrographic characterization of the Upper Ordovician Utica Shale, southern Quebec, Canada

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Cited by 31 publications
(17 citation statements)
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“…With increasing thermal maturity, labile OM (i.e., PC) is transformed to inert/residual carbon (Raiswell and Berner, 1987;Seewald, 2003). Inert carbon composes 98% of OM in overmature deep Utica Shale samples with no further potential for hydrocarbon generation (Haeri-Ardakani et al, 2015). Burial temperatures in the Utica Shale are consistent with measured equivalent vitrinite reflectance (VRo eqv. )…”
Section: Sulfur Stable Isotope Ratios and Distinction Between Msr Andmentioning
confidence: 68%
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“…With increasing thermal maturity, labile OM (i.e., PC) is transformed to inert/residual carbon (Raiswell and Berner, 1987;Seewald, 2003). Inert carbon composes 98% of OM in overmature deep Utica Shale samples with no further potential for hydrocarbon generation (Haeri-Ardakani et al, 2015). Burial temperatures in the Utica Shale are consistent with measured equivalent vitrinite reflectance (VRo eqv. )…”
Section: Sulfur Stable Isotope Ratios and Distinction Between Msr Andmentioning
confidence: 68%
“…Burial temperatures in the Utica Shale are consistent with measured equivalent vitrinite reflectance (VRo eqv. ) values of samples from intermediate (1.24%) and deep wells (2.1%; Haeri-Ardakani et al, 2015) corresponding to burial temperatures between ∼140 to 180 • C.…”
Section: Sulfur Stable Isotope Ratios and Distinction Between Msr Andmentioning
confidence: 99%
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