FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3179370263> ?p ?o ?g. }

• W3179370263 endingPage "106352" @default.
• W3179370263 startingPage "106352" @default.
• W3179370263 abstract "Crustal assimilation and the input of subducted sediment in a subduction zone play vital roles in generating arc and back-arc lavas along a continental margin. However, distinguishing the impacts of these two processes on lava geochemistry is not straightforward or well understood. In this paper, we present new Hf–Nd–Sr–Pb isotopic data for 20 igneous rocks ranging in composition from basalt to rhyolite, which when combined with data from the literature allow us to fingerprint the contributions of crustal and slab-derived materials along the Okinawa Trough (OT). Consistent with previous results, the basaltic lavas were generated by melting of an Indian-type mantle source metasomatised by slab-derived fluids and subducted pelagic/detrital sediments. We confirm that Hf behaves as a non-conservative element during subduction, constrained by Hf-Nd isotopic systematics. Our new data suggest that crustal assimilation processes worked independently of the extent of magma differentiation but were determined by the stage of tectonic development in individual regions. In the southern OT (seafloor spreading stage), crustal assimilation is insignificant, and the addition of subducted sediment is 0.4%–1.5%. In the middle OT (crustal rifting stage), the basaltic and rhyolitic suites do not show distinctive Hf–Nd–Sr–Pb isotopic compositions, and both record moderate crustal assimilation (<10%) and < 0.6% addition of subducted sediment. In contrast, in the southwestern OT (crustal extension stage), the basaltic and dacitic lavas record the highest involvement of 10%–40% crustal material. We conclude that the various stages of back-arc development exerted first-order controls on the extent of crustal assimilation in the OT and had marked effects on the geochemical and isotopic compositions of OT lavas." @default.
• W3179370263 created "2021-07-19" @default.
• W3179370263 creator A5015983532 @default.
• W3179370263 creator A5027228264 @default.
• W3179370263 creator A5032662387 @default.
• W3179370263 creator A5042633188 @default.
• W3179370263 creator A5047036012 @default.
• W3179370263 creator A5048075135 @default.
• W3179370263 creator A5048336770 @default.
• W3179370263 creator A5070828650 @default.
• W3179370263 creator A5086340199 @default.
• W3179370263 creator A5089390321 @default.
• W3179370263 date "2021-10-01" @default.
• W3179370263 modified "2023-09-27" @default.
• W3179370263 title "Hafnium isotopic constraints on crustal assimilation in response to the tectono–magmatic evolution of the Okinawa Trough" @default.
• W3179370263 cites W1566514932 @default.
• W3179370263 cites W1863002528 @default.
• W3179370263 cites W1898579578 @default.
• W3179370263 cites W1910670615 @default.
• W3179370263 cites W1924121559 @default.
• W3179370263 cites W1965853619 @default.
• W3179370263 cites W1969509694 @default.
• W3179370263 cites W1975022665 @default.
• W3179370263 cites W1977911355 @default.
• W3179370263 cites W1982386973 @default.
• W3179370263 cites W1990479851 @default.
• W3179370263 cites W2001131533 @default.
• W3179370263 cites W2004745036 @default.
• W3179370263 cites W2008364272 @default.
• W3179370263 cites W2020468561 @default.
• W3179370263 cites W2021014922 @default.
• W3179370263 cites W2023756316 @default.
• W3179370263 cites W2024443088 @default.
• W3179370263 cites W2026184025 @default.
• W3179370263 cites W2033120385 @default.
• W3179370263 cites W2037054615 @default.
• W3179370263 cites W2037839516 @default.
• W3179370263 cites W2042451718 @default.
• W3179370263 cites W2045085255 @default.
• W3179370263 cites W2047567126 @default.
• W3179370263 cites W2050944272 @default.
• W3179370263 cites W2053315889 @default.
• W3179370263 cites W2054933791 @default.
• W3179370263 cites W2056432227 @default.
• W3179370263 cites W2058709050 @default.
• W3179370263 cites W2059817759 @default.
• W3179370263 cites W2064308056 @default.
• W3179370263 cites W2070071554 @default.
• W3179370263 cites W2077985074 @default.
• W3179370263 cites W2093692135 @default.
• W3179370263 cites W2094234318 @default.
• W3179370263 cites W2096095260 @default.
• W3179370263 cites W2108095642 @default.
• W3179370263 cites W2111184969 @default.
• W3179370263 cites W2117683602 @default.
• W3179370263 cites W2127612728 @default.
• W3179370263 cites W2134360679 @default.
• W3179370263 cites W2138522501 @default.
• W3179370263 cites W2143719562 @default.
• W3179370263 cites W2146745966 @default.
• W3179370263 cites W2148423848 @default.
• W3179370263 cites W2154628848 @default.
• W3179370263 cites W2171161901 @default.
• W3179370263 cites W2191863750 @default.
• W3179370263 cites W2264575613 @default.
• W3179370263 cites W2294609836 @default.
• W3179370263 cites W2341836699 @default.
• W3179370263 cites W2343050077 @default.
• W3179370263 cites W2556355076 @default.
• W3179370263 cites W2564876248 @default.
• W3179370263 cites W2569196174 @default.
• W3179370263 cites W2605265791 @default.
• W3179370263 cites W2606821369 @default.
• W3179370263 cites W2620147810 @default.
• W3179370263 cites W2750918051 @default.
• W3179370263 cites W2790865224 @default.
• W3179370263 cites W2790983425 @default.
• W3179370263 cites W2791649155 @default.
• W3179370263 cites W2793791285 @default.
• W3179370263 cites W2794567058 @default.
• W3179370263 cites W2800783732 @default.
• W3179370263 cites W2892095746 @default.
• W3179370263 cites W2947645303 @default.
• W3179370263 cites W2989810211 @default.
• W3179370263 cites W2992981709 @default.
• W3179370263 cites W3015172104 @default.
• W3179370263 cites W3081630707 @default.
• W3179370263 cites W3085061429 @default.
• W3179370263 cites W3133548150 @default.
• W3179370263 doi "https://doi.org/10.1016/j.lithos.2021.106352" @default.
• W3179370263 hasPublicationYear "2021" @default.
• W3179370263 type Work @default.
• W3179370263 sameAs 3179370263 @default.
• W3179370263 citedByCount "4" @default.
• W3179370263 countsByYear W31793702632021 @default.
• W3179370263 countsByYear W31793702632022 @default.
• W3179370263 countsByYear W31793702632023 @default.
• W3179370263 crossrefType "journal-article" @default.

• next