FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2019040497> ?p ?o ?g. }

• W2019040497 endingPage "128" @default.
• W2019040497 startingPage "110" @default.
• W2019040497 abstract "The Late Permian coals from the Huayingshan Coalfield of southwestern China are significantly enriched in Zr (695 μg/g), Nb (75.9 μg/g), Se (6.99 μg/g), Hf (10.1 μg/g), and rare earth elements and Y (1423 μg/g). Previous studies showed that the sediment-source region for these coals was the Kangdian Upland, which was formed at an early stage of the late Permian Period. The source rocks have a basalt composition, and those studies attributed the enrichment of the above high field strength elements (HFSEs) to derivation from the Kangdian Upland. Geochemical and mineralogical data presented in this study show that the dominant sediment-source regions for the coal and roof strata of the Huayingshan Coalfields are the Dabashan Uplift, Hannan Upland, and Leshan–Longnvsi Uplift. The highly-elevated concentrations of HFSEs in the coals are due to hydrothermal fluids. Three tonstein layers derived from alkali rhyolite were identified. These tonsteins are characterized by highly-enriched HFSEs and by strong negative Eu anomalies in the rare earth element distribution patterns. The major carriers of the rare earth elements in the coal are rhabdophane and silicorhabdophane, the latter of which is also enriched in Zr. Zirconium, however, mainly occurs in zircon. Rhabdophane and silicorhabdophane in the coal are mainly distributed along the bedding planes and occur as cell-fillings. Zircon in the coal occurs as cell-fillings and is of authigenic origin. Anatase in the partings and coals contains Nb, and occurs as fracture-filling and colloidal forms. The modes of occurrence of the above minerals indicate that they were derived from hydrothermal fluids. Mercury and Se mainly occur in sulfide minerals (pyrite and marcasite)." @default.
• W2019040497 created "2016-06-24" @default.
• W2019040497 creator A5001468191 @default.
• W2019040497 creator A5008511971 @default.
• W2019040497 creator A5010913993 @default.
• W2019040497 creator A5010921521 @default.
• W2019040497 creator A5063603492 @default.
• W2019040497 creator A5065333384 @default.
• W2019040497 creator A5080463725 @default.
• W2019040497 creator A5081782443 @default.
• W2019040497 creator A5089110196 @default.
• W2019040497 creator A5091810973 @default.
• W2019040497 date "2014-02-01" @default.
• W2019040497 modified "2023-10-14" @default.
• W2019040497 title "Revisiting the late Permian coal from the Huayingshan, Sichuan, southwestern China: Enrichment and occurrence modes of minerals and trace elements" @default.
• W2019040497 cites W1963971201 @default.
• W2019040497 cites W1979843871 @default.
• W2019040497 cites W1985751354 @default.
• W2019040497 cites W1985825959 @default.
• W2019040497 cites W1988114452 @default.
• W2019040497 cites W1988599772 @default.
• W2019040497 cites W1992292460 @default.
• W2019040497 cites W1993489621 @default.
• W2019040497 cites W2001074362 @default.
• W2019040497 cites W2002999531 @default.
• W2019040497 cites W2007975985 @default.
• W2019040497 cites W2013259970 @default.
• W2019040497 cites W2013867612 @default.
• W2019040497 cites W2014193745 @default.
• W2019040497 cites W2016260972 @default.
• W2019040497 cites W2017723471 @default.
• W2019040497 cites W2019737722 @default.
• W2019040497 cites W2023955945 @default.
• W2019040497 cites W2025067794 @default.
• W2019040497 cites W2028814276 @default.
• W2019040497 cites W2039638835 @default.
• W2019040497 cites W2043621358 @default.
• W2019040497 cites W2046759963 @default.
• W2019040497 cites W2049900380 @default.
• W2019040497 cites W2052260755 @default.
• W2019040497 cites W2053618511 @default.
• W2019040497 cites W2056790688 @default.
• W2019040497 cites W2057063592 @default.
• W2019040497 cites W2059512355 @default.
• W2019040497 cites W2064493626 @default.
• W2019040497 cites W2072306258 @default.
• W2019040497 cites W2078565163 @default.
• W2019040497 cites W2087760823 @default.
• W2019040497 cites W2087796950 @default.
• W2019040497 cites W2091699893 @default.
• W2019040497 cites W2093750105 @default.
• W2019040497 cites W2096891572 @default.
• W2019040497 cites W2099582743 @default.
• W2019040497 cites W2118835828 @default.
• W2019040497 cites W2120423296 @default.
• W2019040497 cites W2127201333 @default.
• W2019040497 cites W2170254659 @default.
• W2019040497 doi "https://doi.org/10.1016/j.coal.2013.12.016" @default.
• W2019040497 hasPublicationYear "2014" @default.
• W2019040497 type Work @default.
• W2019040497 sameAs 2019040497 @default.
• W2019040497 citedByCount "152" @default.
• W2019040497 countsByYear W20190404972014 @default.
• W2019040497 countsByYear W20190404972015 @default.
• W2019040497 countsByYear W20190404972016 @default.
• W2019040497 countsByYear W20190404972017 @default.
• W2019040497 countsByYear W20190404972018 @default.
• W2019040497 countsByYear W20190404972019 @default.
• W2019040497 countsByYear W20190404972020 @default.
• W2019040497 countsByYear W20190404972021 @default.
• W2019040497 countsByYear W20190404972022 @default.
• W2019040497 countsByYear W20190404972023 @default.
• W2019040497 crossrefType "journal-article" @default.
• W2019040497 hasAuthorship W2019040497A5001468191 @default.
• W2019040497 hasAuthorship W2019040497A5008511971 @default.
• W2019040497 hasAuthorship W2019040497A5010913993 @default.
• W2019040497 hasAuthorship W2019040497A5010921521 @default.
• W2019040497 hasAuthorship W2019040497A5063603492 @default.
• W2019040497 hasAuthorship W2019040497A5065333384 @default.
• W2019040497 hasAuthorship W2019040497A5080463725 @default.
• W2019040497 hasAuthorship W2019040497A5081782443 @default.
• W2019040497 hasAuthorship W2019040497A5089110196 @default.
• W2019040497 hasAuthorship W2019040497A5091810973 @default.
• W2019040497 hasConcept C109007969 @default.
• W2019040497 hasConcept C115393850 @default.
• W2019040497 hasConcept C120806208 @default.
• W2019040497 hasConcept C127313418 @default.
• W2019040497 hasConcept C151730666 @default.
• W2019040497 hasConcept C161509811 @default.
• W2019040497 hasConcept C166957645 @default.
• W2019040497 hasConcept C17409809 @default.
• W2019040497 hasConcept C192241223 @default.
• W2019040497 hasConcept C25822816 @default.
• W2019040497 hasConcept C2778849375 @default.
• W2019040497 hasConcept C30370900 @default.
• W2019040497 hasConcept C34682378 @default.
• W2019040497 hasConcept C518851703 @default.
• W2019040497 hasConcept C59235061 @default.

• next