FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2016567279> ?p ?o ?g. }

• W2016567279 endingPage "35" @default.
• W2016567279 startingPage "16" @default.
• W2016567279 abstract "The Gardar failed-rift Province is world-famous for its (per-)alkaline plutonic rocks. Elevated contents of F in the mantle source and F-enrichment in the parental melts have been suggested to account for the peculiarities of the Gardar rocks (e.g. their rare mineralogy, extreme enrichment of HFSE elements, Be or REE in the Ilímaussaq agpaites, and the formation of the unique Ivigtut cryolite deposit). To constrain the formation and chemical evolution of F-bearing melts and fluids, fluorides (fluorite, cryolite, villiaumite, cryolithionite), calcite and siderite from the Ilímaussaq, Motzfeldt and Ivigtut complexes were analysed for their trace element content focusing on the rare earth elements and yttrium (REE). The various generations of fluorite occurring in the granitic Ivigtut, agpaitic Ilímaussaq and miaskitic to agpaitic Motzfeldt intrusions all share a negative Eu anomaly which is attributed to (earlier) feldspar fractionation in the parental alkali basaltic melts. This interpretation is supported by the abundance of anorthositic xenoliths in many Gardar plutonic rocks. The primary magmatic fluorites from Ilímaussaq and Motzfeldt display very similar REE patterns suggesting a formation from closely related parental melts under similar conditions. Hydrothermal fluorites from these intrusions were used to constrain the multiple effects responsible for the incorporation of trace elements into fluorides: temperature dependence, fluid migration/interaction and complexation resulting in REE fractionation. Generally, the REE patterns of Gardar fluorides reflect the evolution and migration of a F/CO2-rich fluid leading to the formation of fluorite and fluorite/calcite veins. In certain units, this fluid inherited the REE patterns of altered host rocks. In addition, there is evidence of an even younger fluid of high REE abundance which resulted in highly variable REE concentrations (up to three orders of magnitude) within one sample of hydrothermal fluorite. The REE patterns of the granitic Ivigtut intrusion show flat to slightly heavy-REE-enriched patterns characterised by a strong tetrad effect. This effect is interpreted to record extensive fluid–rock interaction in highly fractionated, Si-rich systems. Interestingly, the fluorides appear to record different source REE patterns, as the spatially close Motzfeldt and Ilímaussaq intrusions show strong similarities and contrast with the Ivigtut intrusion located 100 km NE. These variations may be attributed to differences in the tectonic position of the intrusions or mantle heterogeneities." @default.
• W2016567279 created "2016-06-24" @default.
• W2016567279 creator A5039513940 @default.
• W2016567279 creator A5048083960 @default.
• W2016567279 creator A5057276671 @default.
• W2016567279 date "2008-01-01" @default.
• W2016567279 modified "2023-09-27" @default.
• W2016567279 title "REE systematics of fluorides, calcite and siderite in peralkaline plutonic rocks from the Gardar Province, South Greenland" @default.
• W2016567279 cites W112581710 @default.
• W2016567279 cites W1586931791 @default.
• W2016567279 cites W1597706934 @default.
• W2016567279 cites W1967554753 @default.
• W2016567279 cites W1968013432 @default.
• W2016567279 cites W1968621514 @default.
• W2016567279 cites W1969859799 @default.
• W2016567279 cites W1977457396 @default.
• W2016567279 cites W1979857165 @default.
• W2016567279 cites W1982560803 @default.
• W2016567279 cites W1983920957 @default.
• W2016567279 cites W1984630236 @default.
• W2016567279 cites W1986430084 @default.
• W2016567279 cites W1988809294 @default.
• W2016567279 cites W1996968686 @default.
• W2016567279 cites W1999708461 @default.
• W2016567279 cites W2002789392 @default.
• W2016567279 cites W2005877813 @default.
• W2016567279 cites W2006510222 @default.
• W2016567279 cites W2009029520 @default.
• W2016567279 cites W2016769560 @default.
• W2016567279 cites W2018418225 @default.
• W2016567279 cites W2024436619 @default.
• W2016567279 cites W2025757764 @default.
• W2016567279 cites W2027969547 @default.
• W2016567279 cites W2031057485 @default.
• W2016567279 cites W2031375188 @default.
• W2016567279 cites W2031908820 @default.
• W2016567279 cites W2033473502 @default.
• W2016567279 cites W2034678763 @default.
• W2016567279 cites W2035283420 @default.
• W2016567279 cites W2038019149 @default.
• W2016567279 cites W2041990018 @default.
• W2016567279 cites W2049705713 @default.
• W2016567279 cites W2050579914 @default.
• W2016567279 cites W2058459535 @default.
• W2016567279 cites W2058924927 @default.
• W2016567279 cites W2064560604 @default.
• W2016567279 cites W2066240400 @default.
• W2016567279 cites W2066423366 @default.
• W2016567279 cites W2071103381 @default.
• W2016567279 cites W2071645790 @default.
• W2016567279 cites W2078410096 @default.
• W2016567279 cites W2084960681 @default.
• W2016567279 cites W2088908220 @default.
• W2016567279 cites W2090886890 @default.
• W2016567279 cites W2091394285 @default.
• W2016567279 cites W2093297848 @default.
• W2016567279 cites W2102598847 @default.
• W2016567279 cites W2107644678 @default.
• W2016567279 cites W2111344340 @default.
• W2016567279 cites W2112052324 @default.
• W2016567279 cites W2119905303 @default.
• W2016567279 cites W2121368895 @default.
• W2016567279 cites W2127641354 @default.
• W2016567279 cites W2131356529 @default.
• W2016567279 cites W2133293870 @default.
• W2016567279 cites W2141664494 @default.
• W2016567279 cites W2148388790 @default.
• W2016567279 cites W2149295856 @default.
• W2016567279 cites W2150603705 @default.
• W2016567279 cites W2154809427 @default.
• W2016567279 cites W2158171625 @default.
• W2016567279 cites W2160448013 @default.
• W2016567279 cites W2162477524 @default.
• W2016567279 cites W2165073556 @default.
• W2016567279 cites W2331233413 @default.
• W2016567279 cites W3027280787 @default.
• W2016567279 cites W3027995714 @default.
• W2016567279 doi "https://doi.org/10.1016/j.chemgeo.2007.10.002" @default.
• W2016567279 hasPublicationYear "2008" @default.
• W2016567279 type Work @default.
• W2016567279 sameAs 2016567279 @default.
• W2016567279 citedByCount "76" @default.
• W2016567279 countsByYear W20165672792012 @default.
• W2016567279 countsByYear W20165672792013 @default.
• W2016567279 countsByYear W20165672792014 @default.
• W2016567279 countsByYear W20165672792015 @default.
• W2016567279 countsByYear W20165672792016 @default.
• W2016567279 countsByYear W20165672792017 @default.
• W2016567279 countsByYear W20165672792018 @default.
• W2016567279 countsByYear W20165672792019 @default.
• W2016567279 countsByYear W20165672792020 @default.
• W2016567279 countsByYear W20165672792021 @default.
• W2016567279 countsByYear W20165672792022 @default.
• W2016567279 countsByYear W20165672792023 @default.
• W2016567279 crossrefType "journal-article" @default.
• W2016567279 hasAuthorship W2016567279A5039513940 @default.
• W2016567279 hasAuthorship W2016567279A5048083960 @default.
• W2016567279 hasAuthorship W2016567279A5057276671 @default.

• next