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- W2095396914 abstract "Abstract Biomaker analyses of oils and source rocks from two anticlinal trends in central Montana (Ragged Point-Ivanhoe-Sumatra, and Big wall-Melstone, respectively) were the key elements in confirming an Upper Mississippian source (Heath formation) for a single family of oils in the Lower Pennsylvanian Tyler sands. For the limestone member of the Heath formation the relative abundances of the various sterane biomarker clases indicate a mesosaline setting. From palaeostructural reconstructions of the present day anticlines [Kranzler I., Bull. Am. Assoc. Pet. Geol. 50 , 2245–2259 (1966)], and considerations of migration routes, oil accumulations occur in the lower Tyler only where the reservoir sands are directly in contact with the limestone member of the Heath formation. The migration of the oil from the Heath formation into the Tyler sands probably did not take place until the late Jurassic or early Cretaceous, until the overburden was great enough for maturation of the Heath source. This would palce time and migration of oil in these two anticlinal trends prior to the uplift of the Central Montana Big Snowy Trough." @default.
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- W2095396914 date "1988-01-01" @default.
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- W2095396914 title "Oil-source studies in central Montana: Correlations and migration implications" @default.
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- W2095396914 doi "https://doi.org/10.1016/0146-6380(88)90058-7" @default.
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