FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2883162410> ?p ?o ?g. }

• W2883162410 endingPage "259" @default.
• W2883162410 startingPage "241" @default.
• W2883162410 abstract "Abstract This research is focused on the characteristics and origin of major authigenic minerals and the influences on the reservoir quality of the Permian Wutonggou Formation sandstones in the eastern slope of Fukang Sag, Junggar Basin, Western China. Authigenic cements were observed and described from thin sections, scanning electron microscopy, fluorescence, and cathodoluminescence. The elemental concentrations of the authigenic minerals were measured by electron probe microanalysis. Additional characterizations were obtained from O and C stable isotope ratios and from the homogenization temperature of aqueous fluid inclusions. The results show that the sandstones in the Wutonggou Formation are dominated by volcanic lithic fragments. Carbonates and laumontites are the major authigenic minerals in the study area. Authigenic quartz and kaolinite can also be observed. Two types of carbonate cements are identified. The first type is calcite with yellow fluorescent hydrocarbon inclusions. The carbon and oxygen isotopes in the calcites are highly C-depleted and O-depleted. The homogenization temperatures of the aqueous fluid inclusions in the calcite cements are higher than the highest paleogeotemperatures during the burial history. Combined with the presence of authigenic fibrous illites and the illitization of kaolinites, it is determined that the precipitation of the calcites is related to the upwelling of deep fluids and was impacted by the CO 2 from the thermal decarboxylation of organic matters during the middle-late Jurassic. The second type is ferroan calcite with blue fluorescent hydrocarbon inclusions and higher contents of Fe, Mn, Cr, and Mg than in the calcites. The ferroan calcites in the Beisantai uplift are rich in 13 C (δ 13 C (V-PDB) values are +22.10‰ and +22.16‰). The precipitation of these ferroan calcites was impacted by the CO 2 from crude oil biodegradation after the late Jurassic. Two types of laumontites are identified. The first type is partially dissolved and is characterized by a high Ca/Na ratio and low Fe contents. The second type is hardly dissolved, has hydrocarbon inclusions with yellow and blue fluorescence, and is characterized by a low Ca/Na ratio and high Fe contents. The first type of laumontite was precipitated prior to hydrocarbon charging and the second type was formed after hydrocarbon charging and meteoric water leaching. The hydration of the volcanic debris provided the source materials for both types of laumontite. The authigenic quartz and kaolinite were formed by the alteration of feldspars, laumontites, and volcanic materials. The evolution of the reservoir properties was impacted by various degrees of cementation and dissolution; as a result, the reservoir quality in the Beisantai uplift was better than in the Shaqiu area." @default.
• W2883162410 created "2018-08-03" @default.
• W2883162410 creator A5003983927 @default.
• W2883162410 creator A5011413537 @default.
• W2883162410 creator A5016451725 @default.
• W2883162410 creator A5017312157 @default.
• W2883162410 creator A5028115428 @default.
• W2883162410 creator A5031777930 @default.
• W2883162410 creator A5055065745 @default.
• W2883162410 creator A5083531522 @default.
• W2883162410 date "2018-11-01" @default.
• W2883162410 modified "2023-10-14" @default.
• W2883162410 title "Characteristics and origin of the major authigenic minerals and their impacts on reservoir quality in the Permian Wutonggou Formation of Fukang Sag, Junggar Basin, western China" @default.
• W2883162410 cites W1547907389 @default.
• W2883162410 cites W1866526036 @default.
• W2883162410 cites W1937181373 @default.
• W2883162410 cites W1964668356 @default.
• W2883162410 cites W1966334417 @default.
• W2883162410 cites W1968700629 @default.
• W2883162410 cites W1982487268 @default.
• W2883162410 cites W1984882841 @default.
• W2883162410 cites W1990881752 @default.
• W2883162410 cites W1991281720 @default.
• W2883162410 cites W1996128165 @default.
• W2883162410 cites W2006990004 @default.
• W2883162410 cites W2008940094 @default.
• W2883162410 cites W2017720481 @default.
• W2883162410 cites W2030790691 @default.
• W2883162410 cites W2031952526 @default.
• W2883162410 cites W2038899946 @default.
• W2883162410 cites W2039246403 @default.
• W2883162410 cites W2042152545 @default.
• W2883162410 cites W2042160113 @default.
• W2883162410 cites W2042299412 @default.
• W2883162410 cites W2043652106 @default.
• W2883162410 cites W2044537972 @default.
• W2883162410 cites W2051295811 @default.
• W2883162410 cites W2057232535 @default.
• W2883162410 cites W2062953728 @default.
• W2883162410 cites W2067825451 @default.
• W2883162410 cites W2069561840 @default.
• W2883162410 cites W2076848342 @default.
• W2883162410 cites W2079159333 @default.
• W2883162410 cites W2085804470 @default.
• W2883162410 cites W2087855081 @default.
• W2883162410 cites W2097523643 @default.
• W2883162410 cites W2099957049 @default.
• W2883162410 cites W2103212151 @default.
• W2883162410 cites W2110527041 @default.
• W2883162410 cites W2110706788 @default.
• W2883162410 cites W2116766931 @default.
• W2883162410 cites W2126925306 @default.
• W2883162410 cites W2135791232 @default.
• W2883162410 cites W2151261306 @default.
• W2883162410 cites W2152171113 @default.
• W2883162410 cites W2169166613 @default.
• W2883162410 cites W2266581500 @default.
• W2883162410 cites W2269989439 @default.
• W2883162410 cites W2277661351 @default.
• W2883162410 cites W2333629708 @default.
• W2883162410 cites W2396913702 @default.
• W2883162410 cites W2486637737 @default.
• W2883162410 cites W2521421706 @default.
• W2883162410 cites W2574820443 @default.
• W2883162410 cites W2591501153 @default.
• W2883162410 cites W2594605921 @default.
• W2883162410 cites W975730588 @default.
• W2883162410 cites W1696710864 @default.
• W2883162410 cites W2071724672 @default.
• W2883162410 doi "https://doi.org/10.1016/j.marpetgeo.2018.07.008" @default.
• W2883162410 hasPublicationYear "2018" @default.
• W2883162410 type Work @default.
• W2883162410 sameAs 2883162410 @default.
• W2883162410 citedByCount "19" @default.
• W2883162410 countsByYear W28831624102019 @default.
• W2883162410 countsByYear W28831624102020 @default.
• W2883162410 countsByYear W28831624102021 @default.
• W2883162410 countsByYear W28831624102022 @default.
• W2883162410 countsByYear W28831624102023 @default.
• W2883162410 crossrefType "journal-article" @default.
• W2883162410 hasAuthorship W2883162410A5003983927 @default.
• W2883162410 hasAuthorship W2883162410A5011413537 @default.
• W2883162410 hasAuthorship W2883162410A5016451725 @default.
• W2883162410 hasAuthorship W2883162410A5017312157 @default.
• W2883162410 hasAuthorship W2883162410A5028115428 @default.
• W2883162410 hasAuthorship W2883162410A5031777930 @default.
• W2883162410 hasAuthorship W2883162410A5055065745 @default.
• W2883162410 hasAuthorship W2883162410A5083531522 @default.
• W2883162410 hasConcept C109007969 @default.
• W2883162410 hasConcept C115393850 @default.
• W2883162410 hasConcept C127313418 @default.
• W2883162410 hasConcept C151730666 @default.
• W2883162410 hasConcept C166957645 @default.
• W2883162410 hasConcept C17409809 @default.
• W2883162410 hasConcept C191935318 @default.
• W2883162410 hasConcept C205649164 @default.
• W2883162410 hasConcept C6494504 @default.
• W2883162410 hasConcept C83365034 @default.

• next