Matches in SemOpenAlex for { <https://semopenalex.org/work/W2341836699> ?p ?o ?g. }
- W2341836699 endingPage "844" @default.
- W2341836699 startingPage "815" @default.
- W2341836699 abstract "Assessing the impact of crustal assimilation on the composition of oceanic arc lavas is important if source composition is to be correctly interpreted. This is particularly the case in the Lesser Antilles where lavas encompass a very large range in radiogenic isotope compositions. Here we present new 176Hf/177Hf and trace element data for a suite of samples from St Lucia in the southern Lesser Antilles arc where assimilation of sediments located within the arc crust has been shown to influence significantly Sr–Nd–Pb isotope compositions. We show that a high rate of assimilation (r = 0·8) of sediment is responsible for the co-variation of Th/Th*, La/Sm, 87Sr/86Sr, 206/207/208Pb/204Pb, 143Nd/144Nd and 176Hf/177Hf towards extreme ‘continental’ compositions. Lavas that escaped sediment assimilation have a typical oceanic arc signature and provide the best indication of mantle source characteristics beneath St Lucia. They display similar Ba/Th, La/Sm and Nd isotopic compositions to lavas further north in the arc, but with slightly more radiogenic Sr and Pb. Addition of less than 2% of local bulk subducting sediment, or less than 3·5% of sediment partial melt or fluid, to the mantle wedge can explain these compositions; these estimates are similar to those previously proposed for the northern arc. After correction for the effects of sediment assimilation, the St Lucia lavas have only slightly more radiogenic Pb and Sr isotope signatures compared with the northern islands; this can be attributed to differences in the isotopic composition of the local subducting sediment rather than to greater sediment input, as has been previously proposed. Comparison of St Lucia with the other southern Lesser Antilles islands suggests that similar mantle source compositions exist beneath Martinique, St Vincent and perhaps Bequia, whereas a more ‘continental’ source might characterize Ile de Caille, Kick ’em Jenny and Grenada." @default.
- W2341836699 created "2016-06-24" @default.
- W2341836699 creator A5000370369 @default.
- W2341836699 creator A5043211204 @default.
- W2341836699 creator A5064410680 @default.
- W2341836699 creator A5080704850 @default.
- W2341836699 creator A5090734880 @default.
- W2341836699 date "2015-04-01" @default.
- W2341836699 modified "2023-10-18" @default.
- W2341836699 title "Seeing through the Effects of Crustal Assimilation to Assess the Source Composition beneath the Southern Lesser Antilles Arc" @default.
- W2341836699 cites W1910670615 @default.
- W2341836699 cites W1965698329 @default.
- W2341836699 cites W1965940748 @default.
- W2341836699 cites W1972256629 @default.
- W2341836699 cites W1973046065 @default.
- W2341836699 cites W1977911355 @default.
- W2341836699 cites W1979178509 @default.
- W2341836699 cites W1982255582 @default.
- W2341836699 cites W1986391626 @default.
- W2341836699 cites W1990479851 @default.
- W2341836699 cites W1992525388 @default.
- W2341836699 cites W1998707404 @default.
- W2341836699 cites W2001126502 @default.
- W2341836699 cites W2007708221 @default.
- W2341836699 cites W2011607179 @default.
- W2341836699 cites W2016018692 @default.
- W2341836699 cites W2019841823 @default.
- W2341836699 cites W2021987309 @default.
- W2341836699 cites W2022980819 @default.
- W2341836699 cites W2024496784 @default.
- W2341836699 cites W2024575502 @default.
- W2341836699 cites W2034250421 @default.
- W2341836699 cites W2037232404 @default.
- W2341836699 cites W2038406687 @default.
- W2341836699 cites W2039517403 @default.
- W2341836699 cites W2049816087 @default.
- W2341836699 cites W2049967021 @default.
- W2341836699 cites W2050141585 @default.
- W2341836699 cites W2057586044 @default.
- W2341836699 cites W2059649426 @default.
- W2341836699 cites W2060289092 @default.
- W2341836699 cites W2063505294 @default.
- W2341836699 cites W2064916534 @default.
- W2341836699 cites W2078840355 @default.
- W2341836699 cites W2079452226 @default.
- W2341836699 cites W2080280169 @default.
- W2341836699 cites W2080843712 @default.
- W2341836699 cites W2083548901 @default.
- W2341836699 cites W2086820683 @default.
- W2341836699 cites W2087052542 @default.
- W2341836699 cites W2092631685 @default.
- W2341836699 cites W2093692135 @default.
- W2341836699 cites W2095681242 @default.
- W2341836699 cites W2107282719 @default.
- W2341836699 cites W2108126573 @default.
- W2341836699 cites W2112737386 @default.
- W2341836699 cites W2119727714 @default.
- W2341836699 cites W2123898634 @default.
- W2341836699 cites W2135879461 @default.
- W2341836699 cites W2145898590 @default.
- W2341836699 cites W2146117929 @default.
- W2341836699 cites W2152669884 @default.
- W2341836699 cites W2156985625 @default.
- W2341836699 cites W2160505034 @default.
- W2341836699 cites W2161272355 @default.
- W2341836699 cites W2171617099 @default.
- W2341836699 cites W4243532865 @default.
- W2341836699 doi "https://doi.org/10.1093/petrology/egv018" @default.
- W2341836699 hasPublicationYear "2015" @default.
- W2341836699 type Work @default.
- W2341836699 sameAs 2341836699 @default.
- W2341836699 citedByCount "28" @default.
- W2341836699 countsByYear W23418366992016 @default.
- W2341836699 countsByYear W23418366992017 @default.
- W2341836699 countsByYear W23418366992018 @default.
- W2341836699 countsByYear W23418366992019 @default.
- W2341836699 countsByYear W23418366992021 @default.
- W2341836699 countsByYear W23418366992022 @default.
- W2341836699 countsByYear W23418366992023 @default.
- W2341836699 crossrefType "journal-article" @default.
- W2341836699 hasAuthorship W2341836699A5000370369 @default.
- W2341836699 hasAuthorship W2341836699A5043211204 @default.
- W2341836699 hasAuthorship W2341836699A5064410680 @default.
- W2341836699 hasAuthorship W2341836699A5080704850 @default.
- W2341836699 hasAuthorship W2341836699A5090734880 @default.
- W2341836699 hasBestOaLocation W23418366991 @default.
- W2341836699 hasConcept C111368507 @default.
- W2341836699 hasConcept C127313418 @default.
- W2341836699 hasConcept C141646446 @default.
- W2341836699 hasConcept C151730666 @default.
- W2341836699 hasConcept C154200439 @default.
- W2341836699 hasConcept C17409809 @default.
- W2341836699 hasConcept C2776698055 @default.
- W2341836699 hasConcept C2816523 @default.
- W2341836699 hasConcept C34682378 @default.
- W2341836699 hasConcept C57016615 @default.
- W2341836699 hasConcept C58097730 @default.
- W2341836699 hasConcept C63379926 @default.