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• W3189179637 abstract "Abstract Geophysical analysis of the Earth's lower mantle has revealed the presence of two superstructures characterized by low shear wave velocities on the core‐mantle boundary. These Large Low Shear Velocity Provinces (LLSVPs) play a crucial role in the dynamics of the lower mantle and act as the source region for deep‐seated mantle plumes. However, their origin, and the characteristics of the surrounding deep mantle, remain enigmatic. Mantle plumes located above the margins of the LLSVPs display evidence for the presence of this deep‐seated, thermally and/or chemically heterogeneous mantle material ascending into the melting region. As a result, analysis of the spatial geochemical heterogeneity in ocean island basalts provides constraints on the structure of the Earth's lower mantle and the origin of the LLSVPs. In this study, we focus on the Galápagos Archipelago in the eastern Pacific, where bilateral asymmetry in the radiogenic isotopic composition of erupted basalts has been linked to the presence of LLSVP material in the underlying plume. We show, using spatial variations in the major element contents of high‐MgO basalts, that the isotopically enriched south‐western region of the Galápagos mantle—assigned to melting of LLSVP material—displays no evidence for lithological heterogeneity in the mantle source. As such, it is unlikely that the Pacific LLSVP represents a pile of subducted oceanic crust. Clear evidence for a lithologically heterogeneous mantle source is, however, found in the north‐central Galápagos, indicating that a recycled crustal component is present near the eastern margin of the Pacific LLSVP, consistent with seismic observations." @default.
• W3189179637 created "2021-08-16" @default.
• W3189179637 creator A5009391224 @default.
• W3189179637 creator A5028054875 @default.
• W3189179637 creator A5028911822 @default.
• W3189179637 creator A5048798917 @default.
• W3189179637 creator A5060925854 @default.
• W3189179637 date "2021-09-01" @default.
• W3189179637 modified "2023-10-17" @default.
• W3189179637 title "Geochemical Constraints on the Structure of the Earth's Deep Mantle and the Origin of the LLSVPs" @default.
• W3189179637 cites W1489504438 @default.
• W3189179637 cites W1503794571 @default.
• W3189179637 cites W1555353126 @default.
• W3189179637 cites W1556940713 @default.
• W3189179637 cites W1659665640 @default.
• W3189179637 cites W1684447970 @default.
• W3189179637 cites W1689232968 @default.
• W3189179637 cites W1765206522 @default.
• W3189179637 cites W1801625845 @default.
• W3189179637 cites W1826084640 @default.
• W3189179637 cites W1873013960 @default.
• W3189179637 cites W1879999282 @default.
• W3189179637 cites W1906914620 @default.
• W3189179637 cites W1914890451 @default.
• W3189179637 cites W1919191558 @default.
• W3189179637 cites W1941456882 @default.
• W3189179637 cites W1957724163 @default.
• W3189179637 cites W1966429735 @default.
• W3189179637 cites W1968430296 @default.
• W3189179637 cites W1969429051 @default.
• W3189179637 cites W1973441493 @default.
• W3189179637 cites W1974463006 @default.
• W3189179637 cites W1974731988 @default.
• W3189179637 cites W1974787630 @default.
• W3189179637 cites W1976213158 @default.
• W3189179637 cites W1977833674 @default.
• W3189179637 cites W1985160890 @default.
• W3189179637 cites W1985525567 @default.
• W3189179637 cites W2003948785 @default.
• W3189179637 cites W2006592158 @default.
• W3189179637 cites W2008782416 @default.
• W3189179637 cites W2015697995 @default.
• W3189179637 cites W2017669289 @default.
• W3189179637 cites W2020425172 @default.
• W3189179637 cites W2021730883 @default.
• W3189179637 cites W2023865085 @default.
• W3189179637 cites W2028824915 @default.
• W3189179637 cites W2030936724 @default.
• W3189179637 cites W2038543720 @default.
• W3189179637 cites W2039067288 @default.
• W3189179637 cites W2045994461 @default.
• W3189179637 cites W2050130236 @default.
• W3189179637 cites W2050271934 @default.
• W3189179637 cites W2052908549 @default.
• W3189179637 cites W2055859870 @default.
• W3189179637 cites W2061351128 @default.
• W3189179637 cites W2067183899 @default.
• W3189179637 cites W2069053606 @default.
• W3189179637 cites W2076197510 @default.
• W3189179637 cites W2080901722 @default.
• W3189179637 cites W2081677058 @default.
• W3189179637 cites W2083691178 @default.
• W3189179637 cites W2087348707 @default.
• W3189179637 cites W2092811366 @default.
• W3189179637 cites W2093159256 @default.
• W3189179637 cites W2094147220 @default.
• W3189179637 cites W2094663134 @default.
• W3189179637 cites W2097676093 @default.
• W3189179637 cites W2101303966 @default.
• W3189179637 cites W2105641900 @default.
• W3189179637 cites W2105919318 @default.
• W3189179637 cites W2108463688 @default.
• W3189179637 cites W2109330186 @default.
• W3189179637 cites W2113821942 @default.
• W3189179637 cites W2114487014 @default.
• W3189179637 cites W2115404639 @default.
• W3189179637 cites W2116593025 @default.
• W3189179637 cites W2124313024 @default.
• W3189179637 cites W2125654971 @default.
• W3189179637 cites W2126985820 @default.
• W3189179637 cites W2131157768 @default.
• W3189179637 cites W2131817581 @default.
• W3189179637 cites W2142050274 @default.
• W3189179637 cites W2142733843 @default.
• W3189179637 cites W2146059010 @default.
• W3189179637 cites W2148501813 @default.
• W3189179637 cites W2153846210 @default.
• W3189179637 cites W2164282238 @default.
• W3189179637 cites W2165247927 @default.
• W3189179637 cites W2169514721 @default.
• W3189179637 cites W2290432715 @default.
• W3189179637 cites W2322371219 @default.
• W3189179637 cites W2326761186 @default.
• W3189179637 cites W2336454346 @default.
• W3189179637 cites W2415875575 @default.
• W3189179637 cites W2474151245 @default.
• W3189179637 cites W2498389000 @default.
• W3189179637 cites W2515049883 @default.
• W3189179637 cites W2566186475 @default.
• W3189179637 cites W2578495124 @default.

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