FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4387669139> ?p ?o ?g. }

• W4387669139 abstract "Abstract A significant deposition of black shales occurred during the Mesoproterozoic Oxygenation Event (MOE). In order to investigate the hydrocarbon generation potential and organic matter enrichment mechanism of these shale deposits, we studied the Xiamaling Formation shale in the North China region as a representative sample of the Mesoproterozoic shale. The research involved organic petrology, organic geochemistry, mineralogy, and elemental geochemistry. The following observations were made: (1) The depositional environment of the Xiamaling Formation shale can be categorized as either oxic or anoxic, with the former having shallow depositional waters and high deposition rates, while the latter has deeper depositional waters and slower deposition rates. (2) Anoxic shales exhibited significantly better hydrocarbon generation potential compared to shales deposited in oxic environments, although the latter still demonstrated high hydrocarbon generation potential. (3) Shales deposited in anoxic environments displayed higher paleoproductivity compared to those deposited in oxic environments. The high deposition rate in oxic environments slowed the decomposition and mineralization of organic matter, leading to the formation of high-quality shales. In contrast, the strong paleoproductivity, along with favorable preservation conditions, accounted for the high hydrocarbon potential of anoxic shales." @default.
• W4387669139 created "2023-10-17" @default.
• W4387669139 creator A5017279581 @default.
• W4387669139 creator A5028018689 @default.
• W4387669139 creator A5047491824 @default.
• W4387669139 creator A5048747742 @default.
• W4387669139 creator A5062310696 @default.
• W4387669139 creator A5080544811 @default.
• W4387669139 creator A5091429059 @default.
• W4387669139 date "2023-10-16" @default.
• W4387669139 modified "2023-10-18" @default.
• W4387669139 title "Hydrocarbon generation potential and organic matter accumulation patterns in organic-rich shale during the mesoproterozoic oxygenation event: evidence from the Xiamaling formation shale" @default.
• W4387669139 cites W1545536250 @default.
• W4387669139 cites W1648236804 @default.
• W4387669139 cites W1965701586 @default.
• W4387669139 cites W1969906605 @default.
• W4387669139 cites W1973595974 @default.
• W4387669139 cites W1979315982 @default.
• W4387669139 cites W1981870881 @default.
• W4387669139 cites W1984797640 @default.
• W4387669139 cites W1994549679 @default.
• W4387669139 cites W1995056746 @default.
• W4387669139 cites W1999626355 @default.
• W4387669139 cites W2001363398 @default.
• W4387669139 cites W2009607369 @default.
• W4387669139 cites W2009839274 @default.
• W4387669139 cites W2010925982 @default.
• W4387669139 cites W2011968190 @default.
• W4387669139 cites W2021651273 @default.
• W4387669139 cites W2038859476 @default.
• W4387669139 cites W2042895971 @default.
• W4387669139 cites W2043144203 @default.
• W4387669139 cites W2043732268 @default.
• W4387669139 cites W2048367190 @default.
• W4387669139 cites W2050188617 @default.
• W4387669139 cites W2057391595 @default.
• W4387669139 cites W2061430449 @default.
• W4387669139 cites W2062218969 @default.
• W4387669139 cites W2062748557 @default.
• W4387669139 cites W2064458124 @default.
• W4387669139 cites W2065620784 @default.
• W4387669139 cites W2083645617 @default.
• W4387669139 cites W2084603288 @default.
• W4387669139 cites W2086386094 @default.
• W4387669139 cites W2087272845 @default.
• W4387669139 cites W2102781407 @default.
• W4387669139 cites W2102947943 @default.
• W4387669139 cites W2108328226 @default.
• W4387669139 cites W2130241233 @default.
• W4387669139 cites W2154305513 @default.
• W4387669139 cites W2161263005 @default.
• W4387669139 cites W2166869273 @default.
• W4387669139 cites W2232460742 @default.
• W4387669139 cites W2265295360 @default.
• W4387669139 cites W2306724485 @default.
• W4387669139 cites W2311835314 @default.
• W4387669139 cites W2417936857 @default.
• W4387669139 cites W2468992164 @default.
• W4387669139 cites W2495771092 @default.
• W4387669139 cites W2496757355 @default.
• W4387669139 cites W2538897227 @default.
• W4387669139 cites W2747587271 @default.
• W4387669139 cites W2766600164 @default.
• W4387669139 cites W2775664285 @default.
• W4387669139 cites W2784344532 @default.
• W4387669139 cites W2902442689 @default.
• W4387669139 cites W2920853690 @default.
• W4387669139 cites W2920932569 @default.
• W4387669139 cites W2955035850 @default.
• W4387669139 cites W2965317269 @default.
• W4387669139 cites W2971543473 @default.
• W4387669139 cites W2973203409 @default.
• W4387669139 cites W3012249689 @default.
• W4387669139 cites W3038832330 @default.
• W4387669139 cites W3041034961 @default.
• W4387669139 cites W3080864428 @default.
• W4387669139 cites W3091081718 @default.
• W4387669139 cites W3095148526 @default.
• W4387669139 cites W3101969639 @default.
• W4387669139 cites W3103148245 @default.
• W4387669139 cites W3160360850 @default.
• W4387669139 cites W3160470923 @default.
• W4387669139 cites W3173522065 @default.
• W4387669139 cites W3193863350 @default.
• W4387669139 cites W3199267888 @default.
• W4387669139 cites W3207517097 @default.
• W4387669139 cites W3210579630 @default.
• W4387669139 cites W3212767055 @default.
• W4387669139 cites W4200053657 @default.
• W4387669139 cites W4205550164 @default.
• W4387669139 cites W4241323086 @default.
• W4387669139 cites W4281732353 @default.
• W4387669139 cites W4284666141 @default.
• W4387669139 cites W4296268532 @default.
• W4387669139 cites W4306932545 @default.
• W4387669139 cites W4309497607 @default.
• W4387669139 cites W4319441099 @default.
• W4387669139 cites W4324142377 @default.
• W4387669139 cites W4361215082 @default.
• W4387669139 doi "https://doi.org/10.1007/s40948-023-00668-3" @default.

• next