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• W2079654964 endingPage "33" @default.
• W2079654964 startingPage "18" @default.
• W2079654964 abstract "To contribute to the understanding of magma evolution in arc settings we investigate the oldest volcanic unit (Kanafià Synthem) of Nisyros volcano, located in the eastern Aegean Sea (Greece). The unit consists of porphyritic pillow lavas of basaltic andesite composition with trace element signatures that are characteristic of island-arc magmas. Two lava types are distinguished on the basis of geochemistry and the presence or absence of xenoliths, with the xenolith-bearing lavas having distinctly elevated Sr, MREE/HREE and MgO/Fe2O3 compared to the xenolith-free lavas. Xenoliths include relatively rare quartzo-feldspathic fragments that represent continental-type material, and coarse clinopyroxenite xenoliths that consist largely of aluminous and calcic clinopyroxene, and accessory aluminous spinel. Anorthite–diopside reaction selvages preserved around the clinopyroxenite xenoliths demonstrate disequilibrium between the xenoliths and the host magma. The xenolith clinopyroxene is distinctly enriched in most lithophile trace elements compared to clinopyroxene phenocrysts in the host magmas. A notable exception is the Sr concentration, which is similar in both clinopyroxene types. The high Al and low Na contents of the clinopyroxenites preclude a cumulate, deep metamorphic, or mantle origin for these xenoliths. Instead, their composition and mineralogy are diagnostic of skarn rocks formed by magma–carbonate interaction in the mid/upper crust. The Kanafià lavas are interpreted to have undergone crystal fractionation, magma mixing/mingling and crustal assimilation while resident in the upper crust. We show that magma–carbonate reaction and associated skarn formation does not necessarily result in easily recognised modification of the melt composition, with the exception of increasing Sr contents. Carbonate assimilation also releases significant CO2, which will likely form a free vapour phase due to the low CO2 solubility of arc magmas. In the broader context, we stress that the effects of carbonate assimilation by arc magma may be more significant than currently recognised. Carbonate assimilation may modify key trace element ratios, such as Sr/Y, in arc magmas, and will liberate significant CO2 as vapour, which may influence eruption dynamics, estimates of subduction zone volatile budgets, and deep mantle CO2 recycling." @default.
• W2079654964 created "2016-06-24" @default.
• W2079654964 creator A5007191033 @default.
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• W2079654964 date "2012-08-01" @default.
• W2079654964 modified "2023-10-03" @default.
• W2079654964 title "Carbonate assimilation during magma evolution at Nisyros (Greece), South Aegean Arc: Evidence from clinopyroxenite xenoliths" @default.
• W2079654964 cites W1592718458 @default.
• W2079654964 cites W1846057075 @default.
• W2079654964 cites W1870310112 @default.
• W2079654964 cites W1957248203 @default.
• W2079654964 cites W1965647955 @default.
• W2079654964 cites W1967910599 @default.
• W2079654964 cites W1969479798 @default.
• W2079654964 cites W1969859799 @default.
• W2079654964 cites W1972256629 @default.
• W2079654964 cites W1972828185 @default.
• W2079654964 cites W1977701399 @default.
• W2079654964 cites W1979066273 @default.
• W2079654964 cites W1979705656 @default.
• W2079654964 cites W1985459640 @default.
• W2079654964 cites W1985963146 @default.
• W2079654964 cites W1988613402 @default.
• W2079654964 cites W1990672888 @default.
• W2079654964 cites W1991234218 @default.
• W2079654964 cites W1992989528 @default.
• W2079654964 cites W1995942773 @default.
• W2079654964 cites W1998707404 @default.
• W2079654964 cites W1999947021 @default.
• W2079654964 cites W2000321590 @default.
• W2079654964 cites W2002822830 @default.
• W2079654964 cites W2005989951 @default.
• W2079654964 cites W2011796119 @default.
• W2079654964 cites W2013629663 @default.
• W2079654964 cites W2021246496 @default.
• W2079654964 cites W2023410884 @default.
• W2079654964 cites W2024494616 @default.
• W2079654964 cites W2026334430 @default.
• W2079654964 cites W2031751752 @default.
• W2079654964 cites W2034252981 @default.
• W2079654964 cites W2034543711 @default.
• W2079654964 cites W2035041137 @default.
• W2079654964 cites W2038230792 @default.
• W2079654964 cites W2038235962 @default.
• W2079654964 cites W2045582465 @default.
• W2079654964 cites W2051829771 @default.
• W2079654964 cites W2052410465 @default.
• W2079654964 cites W2053811841 @default.
• W2079654964 cites W2057013880 @default.
• W2079654964 cites W2057901409 @default.
• W2079654964 cites W2063058129 @default.
• W2079654964 cites W2064329961 @default.
• W2079654964 cites W2069330001 @default.
• W2079654964 cites W2073493889 @default.
• W2079654964 cites W2075534402 @default.
• W2079654964 cites W2077445383 @default.
• W2079654964 cites W2077465161 @default.
• W2079654964 cites W2077916468 @default.
• W2079654964 cites W2078424797 @default.
• W2079654964 cites W2080280169 @default.
• W2079654964 cites W2080368015 @default.
• W2079654964 cites W2082450488 @default.
• W2079654964 cites W2085040685 @default.
• W2079654964 cites W2087011789 @default.
• W2079654964 cites W2089024813 @default.
• W2079654964 cites W2094397084 @default.
• W2079654964 cites W2109277613 @default.
• W2079654964 cites W2117509084 @default.
• W2079654964 cites W2118172271 @default.
• W2079654964 cites W2135077016 @default.
• W2079654964 cites W2139615588 @default.
• W2079654964 cites W2139654255 @default.
• W2079654964 cites W2145385939 @default.
• W2079654964 cites W2152681222 @default.
• W2079654964 cites W2159349162 @default.
• W2079654964 cites W2161787642 @default.
• W2079654964 cites W2313376405 @default.
• W2079654964 cites W2321606097 @default.
• W2079654964 cites W2328010797 @default.
• W2079654964 cites W2334257035 @default.
• W2079654964 cites W2335739744 @default.
• W2079654964 cites W3040847831 @default.
• W2079654964 cites W3207805732 @default.
• W2079654964 doi "https://doi.org/10.1016/j.lithos.2012.04.029" @default.
• W2079654964 hasPublicationYear "2012" @default.
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