FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3148488390> ?p ?o ?g. }

• W3148488390 endingPage "103304" @default.
• W3148488390 startingPage "103304" @default.
• W3148488390 abstract "The Vitória Seamount (VTS), distant ~300 km from the Brazilian coastline at latitude 20°S, is the second closest offshore volcanic complex of the Vitória-Trindade Ridge (VTR) which corresponds to a ca. 1200 km long ridge of seamounts and islands composed of SiO2-undersaturated magmatic rocks commonly considered to be the volcanic track of the Trindade mantle plume in the South American Plate. Based on the first sample dredged from Vitória Seamount, new petrographic and electron microprobe analyses from its rock show an alkaline basalt with pseudotrachytic texture consisting of bytownite and salite phenocrysts, labradorite microliths, anhedral titanomagnetite, and a yellowish green pseudomorphic phase composed of MgO–Al2O3–SiO2–FeO. The fine-grained groundmass is mainly composed of strongly oriented lath-shaped labradorite microliths, opaque minerals, and vesicles filled by a yellowish green pseudomorphic phase. Whole-rock analyses of the Vitória Seamount rock reveal its SiO2 undersaturation (SiO2 ca. 40 wt.%; normative nepheline = 13.8), enrichment in Cr, Co, Ni, V and Sc, along with depletion in Zr, La and Nd contents compared to the other seamounts of the VTR. VTS show a strong enrichment in light-REE (La/SmN ca. 2.68) compared to heavy-REE (La/YbN = 20.79). Major and trace element evidence indicate that the melting of an enriched mantle source to generate the Vitória Seamount magma occurred dominantly in the garnet stability field. Trace element composition of VTS is consistent with ≤ 3% partial melting of the mantle source. Neodymium and Sr isotopic data suggest that the mantle source of the Vitória Seamount had been variably metasomatized by melts derived from enriched mantle component, which may have developed approximately 600 Ma, reconciling with the Brasiliano Orogeny, according to Nd age model. Modeling of the Nd–Sr isotope systematics points out that the primary melt was formed from an asthenospheric mantle (DMM – Depleted MORB [Mid-Ocean Ridge Basalts] Mantle) that underwent mixing with a continentally derived material (represented by EMI [Enriched Mantle I] component). This process can be explained by the mixing of melts from these mantle components during magma genesis." @default.
• W3148488390 created "2021-04-13" @default.
• W3148488390 creator A5010433523 @default.
• W3148488390 creator A5016206125 @default.
• W3148488390 creator A5039457982 @default.
• W3148488390 creator A5044779850 @default.
• W3148488390 creator A5046751306 @default.
• W3148488390 creator A5055475249 @default.
• W3148488390 creator A5055616852 @default.
• W3148488390 creator A5062185658 @default.
• W3148488390 creator A5069004161 @default.
• W3148488390 date "2021-08-01" @default.
• W3148488390 modified "2023-10-17" @default.
• W3148488390 title "First petrologic data for Vitória Seamount, Vitória-Trindade Ridge, South Atlantic: a contribution to the Trindade mantle plume evolution" @default.
• W3148488390 cites W1502173695 @default.
• W3148488390 cites W1964037583 @default.
• W3148488390 cites W1967180730 @default.
• W3148488390 cites W1968287156 @default.
• W3148488390 cites W1969859799 @default.
• W3148488390 cites W1972940669 @default.
• W3148488390 cites W1978262868 @default.
• W3148488390 cites W1985957692 @default.
• W3148488390 cites W1986834399 @default.
• W3148488390 cites W1989175487 @default.
• W3148488390 cites W1989542919 @default.
• W3148488390 cites W1991291552 @default.
• W3148488390 cites W1995857854 @default.
• W3148488390 cites W2011607179 @default.
• W3148488390 cites W2015167263 @default.
• W3148488390 cites W2016020127 @default.
• W3148488390 cites W2017034624 @default.
• W3148488390 cites W2027453112 @default.
• W3148488390 cites W2027862110 @default.
• W3148488390 cites W2030086520 @default.
• W3148488390 cites W2032535444 @default.
• W3148488390 cites W2033300940 @default.
• W3148488390 cites W2034362051 @default.
• W3148488390 cites W2037884619 @default.
• W3148488390 cites W2040092205 @default.
• W3148488390 cites W2051328232 @default.
• W3148488390 cites W2052001189 @default.
• W3148488390 cites W2052900195 @default.
• W3148488390 cites W2070631961 @default.
• W3148488390 cites W2072709625 @default.
• W3148488390 cites W2074649897 @default.
• W3148488390 cites W2078840355 @default.
• W3148488390 cites W2080302864 @default.
• W3148488390 cites W2081224883 @default.
• W3148488390 cites W2086136946 @default.
• W3148488390 cites W2088223235 @default.
• W3148488390 cites W2089645958 @default.
• W3148488390 cites W2089833042 @default.
• W3148488390 cites W2092219906 @default.
• W3148488390 cites W2093878550 @default.
• W3148488390 cites W2095203624 @default.
• W3148488390 cites W2108405651 @default.
• W3148488390 cites W2112438962 @default.
• W3148488390 cites W2113451750 @default.
• W3148488390 cites W2125107304 @default.
• W3148488390 cites W2136039128 @default.
• W3148488390 cites W2137119378 @default.
• W3148488390 cites W2138522501 @default.
• W3148488390 cites W2145191782 @default.
• W3148488390 cites W2149743365 @default.
• W3148488390 cites W2160431324 @default.
• W3148488390 cites W2162462477 @default.
• W3148488390 cites W2178317302 @default.
• W3148488390 cites W2180182746 @default.
• W3148488390 cites W2316030415 @default.
• W3148488390 cites W2316856633 @default.
• W3148488390 cites W2319070632 @default.
• W3148488390 cites W2324661783 @default.
• W3148488390 cites W2326756003 @default.
• W3148488390 cites W2526567822 @default.
• W3148488390 cites W2588395352 @default.
• W3148488390 cites W2604565340 @default.
• W3148488390 cites W2611807881 @default.
• W3148488390 cites W2792033943 @default.
• W3148488390 cites W2897708665 @default.
• W3148488390 cites W2899996211 @default.
• W3148488390 cites W2992113675 @default.
• W3148488390 cites W3000382179 @default.
• W3148488390 cites W3004739173 @default.
• W3148488390 cites W3112338642 @default.
• W3148488390 cites W4237284629 @default.
• W3148488390 cites W4250584844 @default.
• W3148488390 doi "https://doi.org/10.1016/j.jsames.2021.103304" @default.
• W3148488390 hasPublicationYear "2021" @default.
• W3148488390 type Work @default.
• W3148488390 sameAs 3148488390 @default.
• W3148488390 citedByCount "15" @default.
• W3148488390 countsByYear W31484883902021 @default.
• W3148488390 countsByYear W31484883902022 @default.
• W3148488390 countsByYear W31484883902023 @default.
• W3148488390 crossrefType "journal-article" @default.
• W3148488390 hasAuthorship W3148488390A5010433523 @default.
• W3148488390 hasAuthorship W3148488390A5016206125 @default.
• W3148488390 hasAuthorship W3148488390A5039457982 @default.

• next