FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3091876973> ?p ?o ?g. }

• W3091876973 endingPage "904" @default.
• W3091876973 startingPage "904" @default.
• W3091876973 abstract "The Doig Phosphate Zone (DPZ) is a phosphate-bearing marine unit located at the base of the Doig Formation, in the Triassic section of the Western Canada Sedimentary Basin. The DPZ has a maximum thickness of 90 m and extends across northeastern British Columbia and west-central Alberta. In this study, we characterize the significance and interpret the origin of apatite in the DPZ through mineralogical and geochemical analyses, thin section study, and field emission scanning electron microscopy. The occurrence of apatite in the DPZ is not evenly distributed but restricted to discrete 10 to 20 cm thick beds, located near the base of the DPZ. Phosphorites are of two types: grainstones composed primarily of unconformity-bounded coated grains, and intraclastic phosphorites composed of detrital silt-sized grains and apatite coated grains in a cryptocrystalline phosphatic matrix. The phosphorite beds are records of stratigraphic condensation due to low detrital input during transgression. The erosionally truncated phosphatic coated grains and intraclasts are interpreted to be a result of various phases of phosphatization, exhumation, erosion, reworking, winnowing, and redeposition in alternating quiescence and storms or bottom currents. The abundance of pyrite and chalcophile trace elements, as well as the low concentration of proxy elements for organic matter productivity and preservation, are further evidence of stratigraphic condensation, with sulfidic pore water development and extensive organic recycling promoted by biological activity during the long exposure times. The phosphorites were formed under oxygenated water conditions, as suggested by the depletion in Ce and the presence of a diverse benthic fauna." @default.
• W3091876973 created "2020-10-15" @default.
• W3091876973 creator A5002735902 @default.
• W3091876973 creator A5024833425 @default.
• W3091876973 date "2020-10-12" @default.
• W3091876973 modified "2023-09-23" @default.
• W3091876973 title "Significance and Distribution of Apatite in the Triassic Doig Phosphate Zone, Western Canada Sedimentary Basin" @default.
• W3091876973 cites W1509597688 @default.
• W3091876973 cites W1511126766 @default.
• W3091876973 cites W186599913 @default.
• W3091876973 cites W1967392868 @default.
• W3091876973 cites W1975873767 @default.
• W3091876973 cites W1987688882 @default.
• W3091876973 cites W1991299203 @default.
• W3091876973 cites W1995732521 @default.
• W3091876973 cites W2001651429 @default.
• W3091876973 cites W2002018753 @default.
• W3091876973 cites W2002894690 @default.
• W3091876973 cites W2004373591 @default.
• W3091876973 cites W2009558426 @default.
• W3091876973 cites W2010468221 @default.
• W3091876973 cites W2014936152 @default.
• W3091876973 cites W2015633927 @default.
• W3091876973 cites W2040701129 @default.
• W3091876973 cites W2042505381 @default.
• W3091876973 cites W2045375224 @default.
• W3091876973 cites W2049124719 @default.
• W3091876973 cites W2049125299 @default.
• W3091876973 cites W2053153518 @default.
• W3091876973 cites W2054566032 @default.
• W3091876973 cites W2056694533 @default.
• W3091876973 cites W2057391595 @default.
• W3091876973 cites W2060084202 @default.
• W3091876973 cites W2061785747 @default.
• W3091876973 cites W2066200707 @default.
• W3091876973 cites W2077929362 @default.
• W3091876973 cites W2078012795 @default.
• W3091876973 cites W2086361003 @default.
• W3091876973 cites W2120836329 @default.
• W3091876973 cites W2121911562 @default.
• W3091876973 cites W2123805836 @default.
• W3091876973 cites W2137014803 @default.
• W3091876973 cites W2150275801 @default.
• W3091876973 cites W2159367858 @default.
• W3091876973 cites W2163402984 @default.
• W3091876973 cites W2170843958 @default.
• W3091876973 cites W2181434454 @default.
• W3091876973 cites W2182500888 @default.
• W3091876973 cites W2258399182 @default.
• W3091876973 cites W2266330656 @default.
• W3091876973 cites W2476019351 @default.
• W3091876973 cites W2533632061 @default.
• W3091876973 cites W2808689342 @default.
• W3091876973 cites W2902689920 @default.
• W3091876973 cites W2912070616 @default.
• W3091876973 cites W2995007965 @default.
• W3091876973 cites W3006268076 @default.
• W3091876973 cites W3012164516 @default.
• W3091876973 cites W3028939918 @default.
• W3091876973 cites W30614123 @default.
• W3091876973 cites W4249241662 @default.
• W3091876973 doi "https://doi.org/10.3390/min10100904" @default.
• W3091876973 hasPublicationYear "2020" @default.
• W3091876973 type Work @default.
• W3091876973 sameAs 3091876973 @default.
• W3091876973 citedByCount "0" @default.
• W3091876973 crossrefType "journal-article" @default.
• W3091876973 hasAuthorship W3091876973A5002735902 @default.
• W3091876973 hasAuthorship W3091876973A5024833425 @default.
• W3091876973 hasBestOaLocation W30918769731 @default.
• W3091876973 hasConcept C127313418 @default.
• W3091876973 hasConcept C151730666 @default.
• W3091876973 hasConcept C166957645 @default.
• W3091876973 hasConcept C17409809 @default.
• W3091876973 hasConcept C178790620 @default.
• W3091876973 hasConcept C185592680 @default.
• W3091876973 hasConcept C2776062231 @default.
• W3091876973 hasConcept C2777132085 @default.
• W3091876973 hasConcept C2777746296 @default.
• W3091876973 hasConcept C30163351 @default.
• W3091876973 hasConcept C6494504 @default.
• W3091876973 hasConcept C9396515 @default.
• W3091876973 hasConcept C95457728 @default.
• W3091876973 hasConceptScore W3091876973C127313418 @default.
• W3091876973 hasConceptScore W3091876973C151730666 @default.
• W3091876973 hasConceptScore W3091876973C166957645 @default.
• W3091876973 hasConceptScore W3091876973C17409809 @default.
• W3091876973 hasConceptScore W3091876973C178790620 @default.
• W3091876973 hasConceptScore W3091876973C185592680 @default.
• W3091876973 hasConceptScore W3091876973C2776062231 @default.
• W3091876973 hasConceptScore W3091876973C2777132085 @default.
• W3091876973 hasConceptScore W3091876973C2777746296 @default.
• W3091876973 hasConceptScore W3091876973C30163351 @default.
• W3091876973 hasConceptScore W3091876973C6494504 @default.
• W3091876973 hasConceptScore W3091876973C9396515 @default.
• W3091876973 hasConceptScore W3091876973C95457728 @default.
• W3091876973 hasFunder F4320321487 @default.
• W3091876973 hasIssue "10" @default.

• next