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• W2516499820 endingPage "1097" @default.
• W2516499820 startingPage "1079" @default.
• W2516499820 abstract "New major, trace and rare earth element (REE) data, and Sr-Nd isotopic compositions of jadeitite and REE-Hf-O isotopic compositions of zircon in jadeitite of the Syum-Keu ultramafic complex of the Polar Urals are used to constrain its origin and source. The jadeitites have high contents of Na 2 O (12.80–14.56 wt%), Al 2 O 3 (20.30–23.81 wt%), SiO 2 (58.47–59.50 wt%), and are enriched in Sr, Ba, Zr, Hf and depleted in Nb relative to primitive mantle values. Chondrite-normalized REE patterns of the jadeitite display weakly U-shaped distribution patterns, with La N /Yb N ratios of 0.82–2.42, and very weak positive Eu anomalies (δEu = 1.2–1.6). The initial Sr isotopic compositions of the jadeitite range from 0.704000 to 0.703519 ( t = 368 Ma), and the initial Nd-isotope ratios (e Nd = +0.77 to +5.61) differ from those of ancient ocean water, oceanic sediments and eclogite, metagranite, and metasediments in the nearby Marun-Keu complex. Zircons from the jadeitite have variable REE contents (37–587 ppm) and are enriched in HREE, with La CN /Yb CN ratios ranging from 0.001 to 0.01, and Lu CN /Gd CN ratios ranging from 10 to 83. Cerium shows positive anomalies with Ce/Ce* values ranging from 2.8 to 72, and δEu from 0.53 to 1.02. The 176 Hf/ 177 Hf ratios of the zircons range from 0.282708 to 0.283017, with initial Hf isotope compositions ranging from 6.5 to 17.4. These characteristics resemble those of zircons from depleted mantle-derived magmas. The δ 18 O isotope compositions of the zircons range from 5.03‰ to 6.04‰, with an averaged value of 5.45 ± 0.11‰, similar to those of mantle rocks, suggesting that the zircons were acquired from precursor igneous rocks, and then transported and reworked by fluids from the subducting slab. Our new results show that the jadeitite was precipitated from material mainly produced by fluid interaction with mafic-ultramafic rocks in a subduction zone environment." @default.
• W2516499820 created "2016-09-16" @default.
• W2516499820 creator A5003453619 @default.
• W2516499820 creator A5013183498 @default.
• W2516499820 creator A5026257390 @default.
• W2516499820 creator A5028326071 @default.
• W2516499820 creator A5074432258 @default.
• W2516499820 creator A5075909287 @default.
• W2516499820 date "2016-03-07" @default.
• W2516499820 modified "2023-09-27" @default.
• W2516499820 title "Jadeitite in the Syum-Keu ultramafic complex from Polar Urals, Russia: insights intofluid activity in subduction zones" @default.
• W2516499820 cites W1104249897 @default.
• W2516499820 cites W1484329005 @default.
• W2516499820 cites W1491179359 @default.
• W2516499820 cites W1721380001 @default.
• W2516499820 cites W1832899704 @default.
• W2516499820 cites W1847069267 @default.
• W2516499820 cites W1964330823 @default.
• W2516499820 cites W1966312956 @default.
• W2516499820 cites W1967077075 @default.
• W2516499820 cites W1972603973 @default.
• W2516499820 cites W1974518373 @default.
• W2516499820 cites W1976840700 @default.
• W2516499820 cites W1977775146 @default.
• W2516499820 cites W1979082610 @default.
• W2516499820 cites W1987628258 @default.
• W2516499820 cites W1990572818 @default.
• W2516499820 cites W1999166202 @default.
• W2516499820 cites W2001693759 @default.
• W2516499820 cites W2002460023 @default.
• W2516499820 cites W2009739237 @default.
• W2516499820 cites W2025159153 @default.
• W2516499820 cites W2026889131 @default.
• W2516499820 cites W2029365551 @default.
• W2516499820 cites W2030692873 @default.
• W2516499820 cites W2032296023 @default.
• W2516499820 cites W2033051119 @default.
• W2516499820 cites W2033410649 @default.
• W2516499820 cites W2035016526 @default.
• W2516499820 cites W2035145608 @default.
• W2516499820 cites W2036796954 @default.
• W2516499820 cites W2036917391 @default.
• W2516499820 cites W2041895575 @default.
• W2516499820 cites W2046710353 @default.
• W2516499820 cites W2046813960 @default.
• W2516499820 cites W2049797895 @default.
• W2516499820 cites W2053273118 @default.
• W2516499820 cites W2054153355 @default.
• W2516499820 cites W2056764298 @default.
• W2516499820 cites W2058945241 @default.
• W2516499820 cites W2059010589 @default.
• W2516499820 cites W2059854087 @default.
• W2516499820 cites W2061249032 @default.
• W2516499820 cites W2064917868 @default.
• W2516499820 cites W2068907164 @default.
• W2516499820 cites W2069609722 @default.
• W2516499820 cites W2071177829 @default.
• W2516499820 cites W2075450727 @default.
• W2516499820 cites W2075452964 @default.
• W2516499820 cites W2076996184 @default.
• W2516499820 cites W2080325016 @default.
• W2516499820 cites W2081364034 @default.
• W2516499820 cites W2081526255 @default.
• W2516499820 cites W2082696532 @default.
• W2516499820 cites W2089207073 @default.
• W2516499820 cites W2090083374 @default.
• W2516499820 cites W2090206242 @default.
• W2516499820 cites W2090851592 @default.
• W2516499820 cites W2093474148 @default.
• W2516499820 cites W2094643301 @default.
• W2516499820 cites W2095458117 @default.
• W2516499820 cites W2103280364 @default.
• W2516499820 cites W2107016203 @default.
• W2516499820 cites W2110218455 @default.
• W2516499820 cites W2115645707 @default.
• W2516499820 cites W2119921571 @default.
• W2516499820 cites W2132548426 @default.
• W2516499820 cites W2132746247 @default.
• W2516499820 cites W2138522501 @default.
• W2516499820 cites W2139654255 @default.
• W2516499820 cites W2140537472 @default.
• W2516499820 cites W2144065941 @default.
• W2516499820 cites W2146278124 @default.
• W2516499820 cites W2152066361 @default.
• W2516499820 cites W2153926043 @default.
• W2516499820 cites W2155272764 @default.
• W2516499820 cites W2155672073 @default.
• W2516499820 cites W2169076089 @default.
• W2516499820 cites W2314298070 @default.
• W2516499820 cites W2315820422 @default.
• W2516499820 cites W2320317490 @default.
• W2516499820 cites W2326958282 @default.
• W2516499820 cites W2332693454 @default.
• W2516499820 cites W2334501136 @default.
• W2516499820 cites W2375481221 @default.
• W2516499820 cites W3031730757 @default.
• W2516499820 cites W3142400342 @default.
• W2516499820 cites W642057463 @default.

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