FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3203773737> ?p ?o ?g. }

• W3203773737 endingPage "1019" @default.
• W3203773737 startingPage "985" @default.
• W3203773737 abstract "ABSTRACT Pathfinder elements associated with the exploration footprint of the McArthur River unconformity-related U deposit include U, radiogenic Pb, V, Ni, Co, Cu, Mo, As, Zn, and rare earth elements. In this study, the mineralogical and paragenetic context for their occurrence was established by integrating in situ mineral chemistry and laser ablation mass spectrometry chemical mapping of interstitial assemblages, detrital grains, and cements with whole-rock analyses of drill core samples from the diagenetically altered background and the hydrothermally altered sandstone host rocks. Diagenetically altered background sandstones contain a matrix assemblage of illite and dickite, with trace to minor aluminum-phosphate-sulfate (APS) minerals, apatite, and Fe-Ti oxide minerals. Aluminum-phosphate-sulfate minerals account for the majority of the Sr and light rare earth element concentrations, whereas early diagenetic apatite, monazite, and apatite inclusions in detrital quartz and detrital zircon contribute significant U and heavy rare earth elements to samples analyzed with an aggressive leach (partial digestion) such as aqua regia. Hydrothermally altered sandstone host rocks also contain variable assemblages of Al-Mg chlorite (sudoite), alkali-deficient tourmaline, APS minerals, kaolinite, illite, Fe-oxide, and sulfide minerals. Late pre-mineralization chlorite accounts for a significant portion of the observed Ni concentrations, whereas Co, Cu, Mo, and Zn occur predominantly in cryptic sub-micron sulfide and sulfarsenide inclusions within clay mineral aggregates and in association with Fe-Ti oxides. Elevated concentrations of U were observed in cryptic micro-inclusions associated with sulfides in quartz overgrowths, with Fe-Ti oxide micro-inclusions in kaolinite, and in post-mineralization Fe-oxide veins. The distribution of pathfinder elements throughout the deposit footprint appears to be less related to the primary dispersion of alteration minerals from the hydrothermal system than to the secondary dispersion of elements post-mineralization. Their occurrence throughout pre-, syn-, and post-mineralization assemblages further demonstrates the limitations to defining geochemical footprints from pathfinder element concentrations expressed in lithogeochemical data sets without structural, lithological, and mineralogical context." @default.
• W3203773737 created "2021-10-11" @default.
• W3203773737 creator A5008003236 @default.
• W3203773737 creator A5019558955 @default.
• W3203773737 creator A5022583629 @default.
• W3203773737 creator A5031470453 @default.
• W3203773737 creator A5041560159 @default.
• W3203773737 creator A5042158045 @default.
• W3203773737 creator A5044570602 @default.
• W3203773737 creator A5077355218 @default.
• W3203773737 date "2021-09-01" @default.
• W3203773737 modified "2023-09-24" @default.
• W3203773737 title "Alteration mineralogy and pathfinder element inventory in the footprint of the McArthur River unconformity-related uranium deposit, Canada" @default.
• W3203773737 cites W141358841 @default.
• W3203773737 cites W1502018782 @default.
• W3203773737 cites W1964327963 @default.
• W3203773737 cites W1974144355 @default.
• W3203773737 cites W1987734384 @default.
• W3203773737 cites W1990449375 @default.
• W3203773737 cites W1991436008 @default.
• W3203773737 cites W1992515678 @default.
• W3203773737 cites W1994083769 @default.
• W3203773737 cites W2000886616 @default.
• W3203773737 cites W2001481384 @default.
• W3203773737 cites W2002637401 @default.
• W3203773737 cites W2013345827 @default.
• W3203773737 cites W2028401168 @default.
• W3203773737 cites W2031900268 @default.
• W3203773737 cites W2039832638 @default.
• W3203773737 cites W2044621372 @default.
• W3203773737 cites W2045503897 @default.
• W3203773737 cites W2048308230 @default.
• W3203773737 cites W2060064926 @default.
• W3203773737 cites W2063963575 @default.
• W3203773737 cites W2068328836 @default.
• W3203773737 cites W2084648247 @default.
• W3203773737 cites W2086526909 @default.
• W3203773737 cites W2094545984 @default.
• W3203773737 cites W2097330636 @default.
• W3203773737 cites W2097549580 @default.
• W3203773737 cites W2101151824 @default.
• W3203773737 cites W2131513729 @default.
• W3203773737 cites W2163721957 @default.
• W3203773737 cites W2192547039 @default.
• W3203773737 cites W2307274691 @default.
• W3203773737 cites W2465499279 @default.
• W3203773737 cites W2486952936 @default.
• W3203773737 cites W2494321866 @default.
• W3203773737 cites W2551400655 @default.
• W3203773737 cites W2594913662 @default.
• W3203773737 cites W2604481589 @default.
• W3203773737 cites W2619594918 @default.
• W3203773737 cites W267837023 @default.
• W3203773737 cites W2724643597 @default.
• W3203773737 cites W2731120173 @default.
• W3203773737 cites W2739233166 @default.
• W3203773737 cites W2790557546 @default.
• W3203773737 cites W2886269190 @default.
• W3203773737 cites W2890168493 @default.
• W3203773737 cites W2908683941 @default.
• W3203773737 cites W2909616450 @default.
• W3203773737 cites W2910038598 @default.
• W3203773737 cites W2910366613 @default.
• W3203773737 cites W2911127634 @default.
• W3203773737 cites W2950075164 @default.
• W3203773737 cites W2981456417 @default.
• W3203773737 cites W2981598865 @default.
• W3203773737 cites W3030249237 @default.
• W3203773737 cites W3036207339 @default.
• W3203773737 doi "https://doi.org/10.3749/canmin.2000067" @default.
• W3203773737 hasPublicationYear "2021" @default.
• W3203773737 type Work @default.
• W3203773737 sameAs 3203773737 @default.
• W3203773737 citedByCount "1" @default.
• W3203773737 countsByYear W32037737372022 @default.
• W3203773737 crossrefType "journal-article" @default.
• W3203773737 hasAuthorship W3203773737A5008003236 @default.
• W3203773737 hasAuthorship W3203773737A5019558955 @default.
• W3203773737 hasAuthorship W3203773737A5022583629 @default.
• W3203773737 hasAuthorship W3203773737A5031470453 @default.
• W3203773737 hasAuthorship W3203773737A5041560159 @default.
• W3203773737 hasAuthorship W3203773737A5042158045 @default.
• W3203773737 hasAuthorship W3203773737A5044570602 @default.
• W3203773737 hasAuthorship W3203773737A5077355218 @default.
• W3203773737 hasConcept C127313418 @default.
• W3203773737 hasConcept C130452526 @default.
• W3203773737 hasConcept C151730666 @default.
• W3203773737 hasConcept C154401813 @default.
• W3203773737 hasConcept C17409809 @default.
• W3203773737 hasConcept C178790620 @default.
• W3203773737 hasConcept C185592680 @default.
• W3203773737 hasConcept C199289684 @default.
• W3203773737 hasConcept C26687426 @default.
• W3203773737 hasConcept C2776062231 @default.
• W3203773737 hasConcept C2776212575 @default.
• W3203773737 hasConcept C2776268066 @default.
• W3203773737 hasConcept C2777132085 @default.
• W3203773737 hasConcept C2777615417 @default.

• next