FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4385978050> ?p ?o ?g. }

• W4385978050 endingPage "1616" @default.
• W4385978050 startingPage "1616" @default.
• W4385978050 abstract "The hydrocarbon source rocks of the marine carbonates of the Ordovician Majiagou Formation in the Ordos Basin are generally in the high-overmature stage and are, therefore, not suitable for hydrocarbon thermal simulation experiments. Their hydrocarbon generation potential and hydrocarbon generation characteristics are not clearly understood. Meanwhile, Nordic Cambrian carbonates are similar in lithology, parent material type, and sedimentary age, and are in the low evolution stage, which is suitable for hydrocarbon thermal simulation experiments. Therefore, in this study, we selected the Nordic carbonates for the gold tube thermal simulation experiment to analyze the content and geochemical characteristics of the thermal simulation products. The experimental results are also compared and analyzed with the characteristics of thermal simulation products of Pingliang Formation mud shale (contemporaneous with the Majiagou Formation) and Shanxi Formation coal (in the upper part of the Majiagou Formation), which are similar to the Majiagou Formation in the Ordos Basin. The results showed that the Nordic carbonate has different hydrocarbon production characteristics from the mud shale of the Pingliang Formation of the same parent material type, and although the hydrocarbon production yields of the two are not very different, the carbonate still produces methane at 600 °C. The hydrocarbon production yield of the Nordic carbonates is almost equivalent to that of type-II2 kerogen, indicating that the hydrocarbon production yield is not related to lithology and only to the organic matter type; however, the Nordic carbonate can produce a large amount of H2S. The alkane carbon isotope changes are mainly controlled by the degree of thermal evolution, showing gradual heaviness with increasing temperature. No carbon isotope sequence reversal occurred during the thermal simulation, and its distribution range is roughly the same as that of the alkane carbon isotope composition of the mud shale of the Pingliang Formation. The ethane carbon isotope composition is as heavy as −21.2‰ at the high-temperature stage, showing similar coal-type gas characteristics. The addition of calcium sulphate (CaSO4) causes the TSR reaction to occur, which has a significant impact on the methane content under high maturity conditions, reducing its content by more than 50% at 600 °C. However, the addition of CaSO4 increases the yield of heavy hydrocarbon gases, such as ethane, and promotes the production of C6-14 hydrocarbons and C14+ hydrocarbons at high-temperature stages, and the addition of CaSO4 substantially increases the yield of H2, CO2, and H2S. The thermal simulation results have implications for the hydrocarbon formation mechanism of the early Paleozoic marine carbonate formation system in the stacked basins of the Ordos Basin and the Tarim Basin in China." @default.
• W4385978050 created "2023-08-19" @default.
• W4385978050 creator A5007942235 @default.
• W4385978050 creator A5035468538 @default.
• W4385978050 creator A5043365677 @default.
• W4385978050 creator A5043817482 @default.
• W4385978050 creator A5065656010 @default.
• W4385978050 creator A5069598087 @default.
• W4385978050 creator A5072796155 @default.
• W4385978050 date "2023-08-18" @default.
• W4385978050 modified "2023-10-14" @default.
• W4385978050 title "Experimental Characteristics of Hydrocarbon Generation from Scandinavian Alum Shale Carbonate Nodules: Implications for Hydrocarbon Generation from Majiagou Formation Marine Carbonates in China’s Ordos Basin" @default.
• W4385978050 cites W1906510923 @default.
• W4385978050 cites W1963641066 @default.
• W4385978050 cites W1995603005 @default.
• W4385978050 cites W1998591509 @default.
• W4385978050 cites W2008225229 @default.
• W4385978050 cites W2011749218 @default.
• W4385978050 cites W2016237207 @default.
• W4385978050 cites W2022048614 @default.
• W4385978050 cites W2041025309 @default.
• W4385978050 cites W2057277840 @default.
• W4385978050 cites W2062891295 @default.
• W4385978050 cites W2063576167 @default.
• W4385978050 cites W2069196587 @default.
• W4385978050 cites W2079240626 @default.
• W4385978050 cites W2092206175 @default.
• W4385978050 cites W2143094474 @default.
• W4385978050 cites W2328077022 @default.
• W4385978050 cites W2514548830 @default.
• W4385978050 cites W2590965438 @default.
• W4385978050 cites W2620855984 @default.
• W4385978050 cites W2726395512 @default.
• W4385978050 cites W2742192435 @default.
• W4385978050 cites W2783468893 @default.
• W4385978050 cites W2783734142 @default.
• W4385978050 cites W2903098390 @default.
• W4385978050 cites W2931149583 @default.
• W4385978050 cites W2943392095 @default.
• W4385978050 cites W2969589171 @default.
• W4385978050 cites W3081967623 @default.
• W4385978050 cites W3121420613 @default.
• W4385978050 cites W3161299039 @default.
• W4385978050 cites W4224100237 @default.
• W4385978050 cites W4255526734 @default.
• W4385978050 cites W4295886897 @default.
• W4385978050 cites W4296391565 @default.
• W4385978050 cites W4304890564 @default.
• W4385978050 cites W4311843516 @default.
• W4385978050 cites W4319941973 @default.
• W4385978050 cites W4366982730 @default.
• W4385978050 cites W4377861444 @default.
• W4385978050 doi "https://doi.org/10.3390/jmse11081616" @default.
• W4385978050 hasPublicationYear "2023" @default.
• W4385978050 type Work @default.
• W4385978050 citedByCount "0" @default.
• W4385978050 crossrefType "journal-article" @default.
• W4385978050 hasAuthorship W4385978050A5007942235 @default.
• W4385978050 hasAuthorship W4385978050A5035468538 @default.
• W4385978050 hasAuthorship W4385978050A5043365677 @default.
• W4385978050 hasAuthorship W4385978050A5043817482 @default.
• W4385978050 hasAuthorship W4385978050A5065656010 @default.
• W4385978050 hasAuthorship W4385978050A5069598087 @default.
• W4385978050 hasAuthorship W4385978050A5072796155 @default.
• W4385978050 hasBestOaLocation W43859780501 @default.
• W4385978050 hasConcept C109007969 @default.
• W4385978050 hasConcept C122792734 @default.
• W4385978050 hasConcept C126559015 @default.
• W4385978050 hasConcept C127313418 @default.
• W4385978050 hasConcept C151730666 @default.
• W4385978050 hasConcept C153127940 @default.
• W4385978050 hasConcept C17409809 @default.
• W4385978050 hasConcept C178790620 @default.
• W4385978050 hasConcept C185592680 @default.
• W4385978050 hasConcept C191897082 @default.
• W4385978050 hasConcept C192562407 @default.
• W4385978050 hasConcept C19320362 @default.
• W4385978050 hasConcept C199289684 @default.
• W4385978050 hasConcept C2777207669 @default.
• W4385978050 hasConcept C2779196632 @default.
• W4385978050 hasConcept C2780659211 @default.
• W4385978050 hasConcept C6494504 @default.
• W4385978050 hasConcept C91442348 @default.
• W4385978050 hasConceptScore W4385978050C109007969 @default.
• W4385978050 hasConceptScore W4385978050C122792734 @default.
• W4385978050 hasConceptScore W4385978050C126559015 @default.
• W4385978050 hasConceptScore W4385978050C127313418 @default.
• W4385978050 hasConceptScore W4385978050C151730666 @default.
• W4385978050 hasConceptScore W4385978050C153127940 @default.
• W4385978050 hasConceptScore W4385978050C17409809 @default.
• W4385978050 hasConceptScore W4385978050C178790620 @default.
• W4385978050 hasConceptScore W4385978050C185592680 @default.
• W4385978050 hasConceptScore W4385978050C191897082 @default.
• W4385978050 hasConceptScore W4385978050C192562407 @default.
• W4385978050 hasConceptScore W4385978050C19320362 @default.
• W4385978050 hasConceptScore W4385978050C199289684 @default.
• W4385978050 hasConceptScore W4385978050C2777207669 @default.
• W4385978050 hasConceptScore W4385978050C2779196632 @default.

• next