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- W2313539991 abstract "A metabasite lens with eclogite-facies relics discovered within high-grade gneisses, at Punta Orvili (Posada) in NE Sardinia, has proven to be the first example of within-plate basalt among the eclogite-derived, tholeiitic metabasites from the Variscan belt in Sardinia. The composition of the Punta Orvili metabasite is unusual: SiO 2 2 O 3 2 O 3tot >13 wt%, Cr > 550 ppm, Ni > 270 ppm, Mg # 68–70. Detailed investigation of the major and trace element content rules out any significant geochemical modification of the protolith by alteration and/or metamorphic processes. Normative contents of mafic minerals up to 55–79 wt%, very small amounts of Al 2 O 3 and Na 2 O and very high concentrations of MgO, Cr and Ni suggest a protolith of picritic nature. The steeply sloping REE patterns, with La N /Yb N = 13.0–17.3, suggest low-degree partial melting and the presence of garnet, as retention phase of HREE in the mantle source. Enrichment factors are 60–180 times higher for LREE, 30–60 times for MREE, 10–20 times for HREE. The primitive manntle-normalized trace element abundance patterns of the Punta Orvili metabasite show enrichment in Ba, Th, Nb, La, Ce, compared to eclogite-derived metabasites. Values of La/Nb, La/Ta, Ce/Nb, Th/Nb, Sm/Yb, Ce/Sm, Th/Y, Nb/Y, Th/Yb and Ta/Yb differ significantly from those of average crust, upper, lower and mid-crust, indicating an OIB-like source. Two values of 87 Sr/ 86 Sr (i) were obtained around 0.709 with e Sri = +69–71. The corresponding values of the 143 Nd/ 144 Nd (i) are about 0.51197 with e Ndi ~ −1.50 assuming an age of 460 Ma, i.e . the mean age of Sardinian eclogite. Isotope and geochemical data suggest that the Punta Orvili protolith was generated by interaction of OIB-like melts with an enriched sub-continental lithospheric mantle, similar in composition to Group II kimberlites and/or to their garnet peridotite xenoliths." @default.
- W2313539991 created "2016-06-24" @default.
- W2313539991 creator A5005449391 @default.
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- W2313539991 creator A5089245328 @default.
- W2313539991 date "2010-09-09" @default.
- W2313539991 modified "2023-09-25" @default.
- W2313539991 title "Metabasite from the Variscan belt in NE Sardinia, Italy: within-plate OIB-like melts with very high Sr and low Nd isotope ratios" @default.
- W2313539991 cites W1484832768 @default.
- W2313539991 cites W1624806571 @default.
- W2313539991 cites W1636782254 @default.
- W2313539991 cites W1657792928 @default.
- W2313539991 cites W1660289480 @default.
- W2313539991 cites W1928320224 @default.
- W2313539991 cites W1964455314 @default.
- W2313539991 cites W1967004471 @default.
- W2313539991 cites W1967494609 @default.
- W2313539991 cites W1969442201 @default.
- W2313539991 cites W1969859799 @default.
- W2313539991 cites W1971722259 @default.
- W2313539991 cites W1973012528 @default.
- W2313539991 cites W1974613213 @default.
- W2313539991 cites W1974731988 @default.
- W2313539991 cites W1979790829 @default.
- W2313539991 cites W1981328102 @default.
- W2313539991 cites W1983244355 @default.
- W2313539991 cites W1987968639 @default.
- W2313539991 cites W1988251519 @default.
- W2313539991 cites W1988694196 @default.
- W2313539991 cites W1990091620 @default.
- W2313539991 cites W2008373173 @default.
- W2313539991 cites W2009544440 @default.
- W2313539991 cites W2010964930 @default.
- W2313539991 cites W2013952426 @default.
- W2313539991 cites W2014742538 @default.
- W2313539991 cites W2015880584 @default.
- W2313539991 cites W2015957834 @default.
- W2313539991 cites W2016383875 @default.
- W2313539991 cites W2017750787 @default.
- W2313539991 cites W2019027482 @default.
- W2313539991 cites W2021129207 @default.
- W2313539991 cites W2025739137 @default.
- W2313539991 cites W2035167665 @default.
- W2313539991 cites W2036255513 @default.
- W2313539991 cites W2040660011 @default.
- W2313539991 cites W2041112329 @default.
- W2313539991 cites W2050130236 @default.
- W2313539991 cites W2055179278 @default.
- W2313539991 cites W2057289988 @default.
- W2313539991 cites W2057834112 @default.
- W2313539991 cites W2058174271 @default.
- W2313539991 cites W2058578055 @default.
- W2313539991 cites W2058717414 @default.
- W2313539991 cites W2060747257 @default.
- W2313539991 cites W2062052372 @default.
- W2313539991 cites W2063705096 @default.
- W2313539991 cites W2077698686 @default.
- W2313539991 cites W2082832653 @default.
- W2313539991 cites W2086088951 @default.
- W2313539991 cites W2090194751 @default.
- W2313539991 cites W2094709181 @default.
- W2313539991 cites W2094806449 @default.
- W2313539991 cites W2095519914 @default.
- W2313539991 cites W2097044248 @default.
- W2313539991 cites W2098027691 @default.
- W2313539991 cites W2098071006 @default.
- W2313539991 cites W2100958416 @default.
- W2313539991 cites W2107651481 @default.
- W2313539991 cites W2111696978 @default.
- W2313539991 cites W2113451750 @default.
- W2313539991 cites W2127236625 @default.
- W2313539991 cites W2127582882 @default.
- W2313539991 cites W2129949055 @default.
- W2313539991 cites W2130520939 @default.
- W2313539991 cites W2135330428 @default.
- W2313539991 cites W2135916666 @default.
- W2313539991 cites W2138522501 @default.
- W2313539991 cites W2139950654 @default.
- W2313539991 cites W2141890535 @default.
- W2313539991 cites W2146435019 @default.
- W2313539991 cites W2148835780 @default.
- W2313539991 cites W2164294319 @default.
- W2313539991 cites W2165545174 @default.
- W2313539991 cites W2166978438 @default.
- W2313539991 cites W2168242075 @default.
- W2313539991 cites W2185965248 @default.
- W2313539991 cites W2315895345 @default.
- W2313539991 cites W2321354652 @default.
- W2313539991 cites W2321359132 @default.
- W2313539991 cites W2326076458 @default.
- W2313539991 cites W2914239990 @default.
- W2313539991 doi "https://doi.org/10.1127/0935-1221/2010/0022-2042" @default.
- W2313539991 hasPublicationYear "2010" @default.
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