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• W2110631073 endingPage "1557" @default.
• W2110631073 startingPage "1533" @default.
• W2110631073 abstract "We have performed reaction experiments between 1, 4, and 5 wt % CO2-bearing MORB-eclogite (recycled oceanic crust)-derived low-degree andesitic partial melt and fertile peridotite at 1375°C, 3 GPa for infiltrating melt fractions of 25% and 33% by weight. We observe that the reacted melts are alkalic with degree of alkalinity or Si undersaturation increasing with increasing CO2 content in reacting melt. Consequently, an andesite evolves through basanite to nephelinite owing to greater drawdown of SiO2 from melt and enhanced precipitation of orthopyroxene in residue. We have developed an empirical model to predict reacted melt composition as a function of reacting andesite fraction and source CO2 concentration. Using our model, we have quantified the mutual proportions of equilibrated melt from andesite-peridotite (+ CO2) hybridization and subsequent peridotite (± CO2)-derived melt required to produce the major element composition of various ocean island basalts. Our model can thus be applied to characterize the source of ocean islands from primary alkalic lava composition. Accordingly, we determined that average HIMU source requires 24 wt % of MORB-eclogite-derived melt relative to peridotite containing 2 wt % CO2 and subsequent contribution of 45% of volatile-free peridotite partial melt. We demonstrate that mantle hybridization by eclogite melt-peridotite (± CO2) reaction in the system can produce high MgO (>15 wt %) basaltic melts at mantle potential temperature (TP) of 1350°C. Therefore, currently used thermometers to estimate TP using MgO content of primary alkalic melts need to be revised, with corrections for melt-rock reaction in a heterogeneous mantle as well as presence of CO2." @default.
• W2110631073 created "2016-06-24" @default.
• W2110631073 creator A5043563326 @default.
• W2110631073 creator A5081619254 @default.
• W2110631073 date "2014-04-01" @default.
• W2110631073 modified "2023-09-30" @default.
• W2110631073 title "Effect of variable CO₂on eclogite-derived andesite and lherzolite reaction at 3 GPa-Implications for mantle source characteristics of alkalic ocean island basalts" @default.
• W2110631073 cites W1507573241 @default.
• W2110631073 cites W1532991590 @default.
• W2110631073 cites W1879999282 @default.
• W2110631073 cites W1966397334 @default.
• W2110631073 cites W1969735264 @default.
• W2110631073 cites W1971515643 @default.
• W2110631073 cites W1971617122 @default.
• W2110631073 cites W1972352700 @default.
• W2110631073 cites W1972385086 @default.
• W2110631073 cites W1974231715 @default.
• W2110631073 cites W1977438826 @default.
• W2110631073 cites W1978801698 @default.
• W2110631073 cites W1978978739 @default.
• W2110631073 cites W1979503354 @default.
• W2110631073 cites W1981378138 @default.
• W2110631073 cites W1981883491 @default.
• W2110631073 cites W1983316554 @default.
• W2110631073 cites W1990519851 @default.
• W2110631073 cites W1990672407 @default.
• W2110631073 cites W1992456608 @default.
• W2110631073 cites W1993661498 @default.
• W2110631073 cites W1996202067 @default.
• W2110631073 cites W2000098146 @default.
• W2110631073 cites W2000191403 @default.
• W2110631073 cites W2002193431 @default.
• W2110631073 cites W2002975639 @default.
• W2110631073 cites W2003948785 @default.
• W2110631073 cites W2004474671 @default.
• W2110631073 cites W2004856555 @default.
• W2110631073 cites W2005647481 @default.
• W2110631073 cites W2008782416 @default.
• W2110631073 cites W2013131631 @default.
• W2110631073 cites W2024141736 @default.
• W2110631073 cites W2024241034 @default.
• W2110631073 cites W2027293310 @default.
• W2110631073 cites W2029330897 @default.
• W2110631073 cites W2040637635 @default.
• W2110631073 cites W2042832983 @default.
• W2110631073 cites W2043466950 @default.
• W2110631073 cites W2046141409 @default.
• W2110631073 cites W2052473341 @default.
• W2110631073 cites W2055859870 @default.
• W2110631073 cites W2056910670 @default.
• W2110631073 cites W2059197455 @default.
• W2110631073 cites W2065110050 @default.
• W2110631073 cites W2067203284 @default.
• W2110631073 cites W2069173262 @default.
• W2110631073 cites W2073456062 @default.
• W2110631073 cites W2073493889 @default.
• W2110631073 cites W2075818091 @default.
• W2110631073 cites W2076755830 @default.
• W2110631073 cites W2077430827 @default.
• W2110631073 cites W2081640236 @default.
• W2110631073 cites W2081677058 @default.
• W2110631073 cites W2081958168 @default.
• W2110631073 cites W2082442505 @default.
• W2110631073 cites W2083691178 @default.
• W2110631073 cites W2084620534 @default.
• W2110631073 cites W2086540936 @default.
• W2110631073 cites W2089705432 @default.
• W2110631073 cites W2090345767 @default.
• W2110631073 cites W2095477653 @default.
• W2110631073 cites W2100995592 @default.
• W2110631073 cites W2101303966 @default.
• W2110631073 cites W2109170608 @default.
• W2110631073 cites W2111277048 @default.
• W2110631073 cites W2113840820 @default.
• W2110631073 cites W2115653418 @default.
• W2110631073 cites W2120471746 @default.
• W2110631073 cites W2125654971 @default.
• W2110631073 cites W2128673582 @default.
• W2110631073 cites W2133103627 @default.
• W2110631073 cites W2134504371 @default.
• W2110631073 cites W2136039128 @default.
• W2110631073 cites W2147283649 @default.
• W2110631073 cites W2148501813 @default.
• W2110631073 cites W2149565897 @default.
• W2110631073 cites W2151041036 @default.
• W2110631073 cites W2156212191 @default.
• W2110631073 cites W2167782460 @default.
• W2110631073 cites W2322277438 @default.
• W2110631073 cites W2334608288 @default.
• W2110631073 cites W4214911971 @default.
• W2110631073 cites W4248689598 @default.
• W2110631073 doi "https://doi.org/10.1002/2014gc005251" @default.
• W2110631073 hasPublicationYear "2014" @default.
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