1986
DOI: 10.1016/0168-9622(86)90022-9
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Laboratory-simulated thermal maturation of different types of sediments from the Williston Basin, North America—effects on the production rates, the isotopic and organo-geochemical composition of various pyrolysis products

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Cited by 21 publications
(11 citation statements)
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“…10) and, therefore, with distance from Rote Fäule, argues for the preferential release of 12 C-rich organic constituents during oxidative alteration of organic matter as indicated by the organic geochemistry data discussed previously. Consequently, the residual organic matter is enriched in 13 C (Arneth and Matzigkeit 1986). The results are in agreement with the carbon isotopic trend obtained from Kupferschiefer profiles of the Richelsdorf Hills in Germany (Bechtel and Püttmann 1991).…”
Section: Carbon Isotopic Analysis Of Organic Mattersupporting
confidence: 89%
“…10) and, therefore, with distance from Rote Fäule, argues for the preferential release of 12 C-rich organic constituents during oxidative alteration of organic matter as indicated by the organic geochemistry data discussed previously. Consequently, the residual organic matter is enriched in 13 C (Arneth and Matzigkeit 1986). The results are in agreement with the carbon isotopic trend obtained from Kupferschiefer profiles of the Richelsdorf Hills in Germany (Bechtel and Püttmann 1991).…”
Section: Carbon Isotopic Analysis Of Organic Mattersupporting
confidence: 89%
“…The 3 13 C results in Table 3 underscore the well-known isotopic disproportionation of sedimentary organic carbon during thermal maturation into 13 C-depleted low-molecular hydrocarbon compounds and relatively 13 C-enriched remaining kerogen, as documented from anhydrous pyrolysis (Sackett, 1978;Peters et al, 1981;Arneth and Matzigkeit, 1986; reviewed by Whiticar, 1996), hydrous pyrolysis (Andresen et al, 1995;E li l 1995) pyrolysis of a Green River Fm. shale sample similar to the one used in this study (Collister et al, 1992).…”
Section: Methodsmentioning
confidence: 95%
“…Following artificial pyrolysis in the laboratory, residual kerogen type III and other types of organic matter were 13 C-depleted by 1.9-3.0& relative to organic pyrolysates (Arneth and Matzigkeit, 1986). The same authors observed a decreasing d 13 C trend for a type III kerogen with increasing thermal stress.…”
Section: C Shifts In Thermally Maturing Kerogenmentioning
confidence: 90%