FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3036321567> ?p ?o ?g. }

• W3036321567 endingPage "1032" @default.
• W3036321567 startingPage "1028" @default.
• W3036321567 abstract "Abstract The Archean continental lithosphere consists of a dominantly felsic continental crust, made of tonalite-trondhjemite-granodiorite (TTG) and subordinate granitoids, and a cratonic lithospheric mantle, made of highly refractory peridotites. Whether they stemmed from the same process of differentiation from the primitive mantle, or were two distinct components that were physically juxtaposed, remains debated. Metal stable isotope ratios are sensitive to magmatic and metamorphic processes and do not evolve with time. Therefore, stable isotope ratios are complementary to radiogenic isotope ratios, and they allow direct comparisons to be made between different terrestrial components without age corrections. Isotopes of iron and zinc, metals ubiquitous in Earth’s lithosphere, can be tracers of lithospheric formation and evolution because they are affected by partial melting (Fe, Zn), redox state (Fe), and the presence of sulfides (Fe, Zn). Here, using stable Fe and Zn isotopic data from Archean samples of the lithospheric mantle and the continental crust, we show that Fe and Zn isotopes define a linear array, best explained by their coupled fractionation behavior during magmatic processes. Our data show that high degrees of partial melting (&gt;30%) during the formation of the cratonic mantle and mafic protocrust, and reworking of the early crust significantly fractionate Fe and Zn isotopes. Conversely, Fe and Zn isotope ratios in the TTG are similar to those in Archean mafic rocks, suggesting an origin by fractional crystallization of basalt, and implying limited Fe and Zn isotopic fractionation, instead of partial melting of mafic crust. Moreover, the absence of Fe and Zn isotope decoupling due to redox effects, melt (fluid)–rock or sediment-rock interaction, and decarbonation indicates that subduction, at least as we understand it now, is not required to explain the Fe and Zn isotope composition of the Archean lithosphere." @default.
• W3036321567 created "2020-06-25" @default.
• W3036321567 creator A5000079226 @default.
• W3036321567 creator A5008575251 @default.
• W3036321567 creator A5036352635 @default.
• W3036321567 creator A5071655750 @default.
• W3036321567 creator A5074052889 @default.
• W3036321567 creator A5075762231 @default.
• W3036321567 date "2020-06-19" @default.
• W3036321567 modified "2023-09-26" @default.
• W3036321567 title "Archean lithospheric differentiation: Insights from Fe and Zn isotopes" @default.
• W3036321567 cites W1799570852 @default.
• W3036321567 cites W1964175282 @default.
• W3036321567 cites W1964490562 @default.
• W3036321567 cites W1995194566 @default.
• W3036321567 cites W2007377958 @default.
• W3036321567 cites W2043150294 @default.
• W3036321567 cites W2050020771 @default.
• W3036321567 cites W2055172418 @default.
• W3036321567 cites W2060960349 @default.
• W3036321567 cites W2071069131 @default.
• W3036321567 cites W2072620570 @default.
• W3036321567 cites W2085234182 @default.
• W3036321567 cites W2091065826 @default.
• W3036321567 cites W2119330075 @default.
• W3036321567 cites W2257736499 @default.
• W3036321567 cites W2478962634 @default.
• W3036321567 cites W2513789484 @default.
• W3036321567 cites W2537284114 @default.
• W3036321567 cites W2556678425 @default.
• W3036321567 cites W2587710731 @default.
• W3036321567 cites W2622948098 @default.
• W3036321567 cites W2721923203 @default.
• W3036321567 cites W2753858913 @default.
• W3036321567 cites W2768477026 @default.
• W3036321567 cites W2772963007 @default.
• W3036321567 cites W2805038882 @default.
• W3036321567 cites W2883541920 @default.
• W3036321567 cites W2914753986 @default.
• W3036321567 cites W2916725444 @default.
• W3036321567 cites W2918321192 @default.
• W3036321567 cites W2936118752 @default.
• W3036321567 cites W2998878292 @default.
• W3036321567 cites W3000463563 @default.
• W3036321567 doi "https://doi.org/10.1130/g47647.1" @default.
• W3036321567 hasPublicationYear "2020" @default.
• W3036321567 type Work @default.
• W3036321567 sameAs 3036321567 @default.
• W3036321567 citedByCount "18" @default.
• W3036321567 countsByYear W30363215672021 @default.
• W3036321567 countsByYear W30363215672022 @default.
• W3036321567 countsByYear W30363215672023 @default.
• W3036321567 crossrefType "journal-article" @default.
• W3036321567 hasAuthorship W3036321567A5000079226 @default.
• W3036321567 hasAuthorship W3036321567A5008575251 @default.
• W3036321567 hasAuthorship W3036321567A5036352635 @default.
• W3036321567 hasAuthorship W3036321567A5071655750 @default.
• W3036321567 hasAuthorship W3036321567A5074052889 @default.
• W3036321567 hasAuthorship W3036321567A5075762231 @default.
• W3036321567 hasConcept C11872896 @default.
• W3036321567 hasConcept C121332964 @default.
• W3036321567 hasConcept C127313418 @default.
• W3036321567 hasConcept C141646446 @default.
• W3036321567 hasConcept C149347711 @default.
• W3036321567 hasConcept C151730666 @default.
• W3036321567 hasConcept C164304813 @default.
• W3036321567 hasConcept C167284885 @default.
• W3036321567 hasConcept C16942324 @default.
• W3036321567 hasConcept C17409809 @default.
• W3036321567 hasConcept C193429443 @default.
• W3036321567 hasConcept C2776698055 @default.
• W3036321567 hasConcept C2779334269 @default.
• W3036321567 hasConcept C62520636 @default.
• W3036321567 hasConcept C67236022 @default.
• W3036321567 hasConcept C77928131 @default.
• W3036321567 hasConcept C79572550 @default.
• W3036321567 hasConceptScore W3036321567C11872896 @default.
• W3036321567 hasConceptScore W3036321567C121332964 @default.
• W3036321567 hasConceptScore W3036321567C127313418 @default.
• W3036321567 hasConceptScore W3036321567C141646446 @default.
• W3036321567 hasConceptScore W3036321567C149347711 @default.
• W3036321567 hasConceptScore W3036321567C151730666 @default.
• W3036321567 hasConceptScore W3036321567C164304813 @default.
• W3036321567 hasConceptScore W3036321567C167284885 @default.
• W3036321567 hasConceptScore W3036321567C16942324 @default.
• W3036321567 hasConceptScore W3036321567C17409809 @default.
• W3036321567 hasConceptScore W3036321567C193429443 @default.
• W3036321567 hasConceptScore W3036321567C2776698055 @default.
• W3036321567 hasConceptScore W3036321567C2779334269 @default.
• W3036321567 hasConceptScore W3036321567C62520636 @default.
• W3036321567 hasConceptScore W3036321567C67236022 @default.
• W3036321567 hasConceptScore W3036321567C77928131 @default.
• W3036321567 hasConceptScore W3036321567C79572550 @default.
• W3036321567 hasIssue "10" @default.
• W3036321567 hasLocation W30363215671 @default.
• W3036321567 hasLocation W30363215672 @default.
• W3036321567 hasLocation W30363215673 @default.
• W3036321567 hasOpenAccess W3036321567 @default.

• next