FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2419258853> ?p ?o ?g. }

• W2419258853 endingPage "381" @default.
• W2419258853 startingPage "367" @default.
• W2419258853 abstract "Abstract Nelsonite and Fe–Ti oxides ore are common in Proterozoic massif-type anorthosites and layered intrusions. Their geneses have long been controversial, with existing hypotheses including liquid immiscibility between Si-rich and Fe–Ti–P-rich melts and gravitational fractionation among apatite, magnetite, ilmenite and silicates. In this paper, we report detailed field geology and mineral geochemical studies of the nelsonite and Fe–Ti oxides ore from the Damiao anorthosite complex, NE China. Geological observations indicate that the nelsonite and Fe–Ti oxides ore occur as irregularly inclined stratiform-like or lensoid or veins, and are in sharp contact with the anorthosite and gabbronorite. The widespread veins and lenses structure of the Damiao nelsonite and Fe–Ti oxides ore in the anorthosite indicates their immiscibility-derived origin. The apatite in the nelsonite and gabbronorite shows evolution trends different from that in the gabbronorite in the diagrams of Sr versus REEs and Eu/Eu*, suggesting that petrogenesis of the nelsonite and gabbronorite is different from the gabbronorite. Compared with the gabbronorite, the nelsonite and Fe–Ti oxides ore have magnetite high in Cr, plagioclase high in Sr and low in An, and apatite high in Sr, low in REEs with negative Eu anomaly. The evidence permits us to propose that the Damiao Fe–Ti oxides ore/nelsonite and gabbronorite were derived from different parental magmas. The gabbronorite was formed by solidification of the interstitial ferrodioritic magma in the anorthosite, which was the residual magma after extensive plagioclase and pyroxene crystallization and was carried upward by the plagioclase crystal mesh. In contrast, the Fe–Ti oxides ore and nelsonites and mangerite were produced by crystallization of the Fe–Ti–P-rich and SiO2-rich magmas, respectively, due to the liquid immiscibility that occurred when the highly evolved ferrodioritic magma mixed with newly replenished magmas. The variation from Fe–Ti oxides ore to nelsonite and gabbro-nelsonite upwards (as apatite content increases with height) in the steeply inclined Fe–Ti oxides orebodies suggest that gravity fractionation may have played important roles during the crystallization of the Fe–Ti–P-rich magma." @default.
• W2419258853 created "2016-06-24" @default.
• W2419258853 creator A5011065438 @default.
• W2419258853 creator A5029695428 @default.
• W2419258853 creator A5062195279 @default.
• W2419258853 creator A5066742396 @default.
• W2419258853 creator A5069687620 @default.
• W2419258853 creator A5071418521 @default.
• W2419258853 creator A5090034308 @default.
• W2419258853 date "2016-12-01" @default.
• W2419258853 modified "2023-10-01" @default.
• W2419258853 title "Origin of nelsonite and Fe–Ti oxides ore of the Damiao anorthosite complex, NE China: Evidence from trace element geochemistry of apatite, plagioclase, magnetite and ilmenite" @default.
• W2419258853 cites W1618437740 @default.
• W2419258853 cites W1675648967 @default.
• W2419258853 cites W1829255269 @default.
• W2419258853 cites W1968405128 @default.
• W2419258853 cites W1970122979 @default.
• W2419258853 cites W1973144803 @default.
• W2419258853 cites W1976264605 @default.
• W2419258853 cites W1977676766 @default.
• W2419258853 cites W1978486812 @default.
• W2419258853 cites W1979782827 @default.
• W2419258853 cites W1981887323 @default.
• W2419258853 cites W1985097546 @default.
• W2419258853 cites W1995533397 @default.
• W2419258853 cites W2001717205 @default.
• W2419258853 cites W2007332617 @default.
• W2419258853 cites W2008864389 @default.
• W2419258853 cites W2009282737 @default.
• W2419258853 cites W2018366877 @default.
• W2419258853 cites W2019853189 @default.
• W2419258853 cites W2019940244 @default.
• W2419258853 cites W2025213759 @default.
• W2419258853 cites W2032317029 @default.
• W2419258853 cites W2036710144 @default.
• W2419258853 cites W2037945166 @default.
• W2419258853 cites W2069480477 @default.
• W2419258853 cites W2070437901 @default.
• W2419258853 cites W2105740241 @default.
• W2419258853 cites W2120457265 @default.
• W2419258853 cites W2122827719 @default.
• W2419258853 cites W2127083348 @default.
• W2419258853 cites W2133042542 @default.
• W2419258853 cites W2138522501 @default.
• W2419258853 cites W2145463664 @default.
• W2419258853 cites W2147118259 @default.
• W2419258853 cites W2148945411 @default.
• W2419258853 cites W2156333576 @default.
• W2419258853 cites W2159917117 @default.
• W2419258853 cites W2159940268 @default.
• W2419258853 cites W2161729494 @default.
• W2419258853 cites W2163144293 @default.
• W2419258853 cites W2164517911 @default.
• W2419258853 cites W2165712457 @default.
• W2419258853 cites W2171153552 @default.
• W2419258853 cites W2171801505 @default.
• W2419258853 cites W2316589109 @default.
• W2419258853 cites W2330204384 @default.
• W2419258853 cites W2330897866 @default.
• W2419258853 cites W2471616303 @default.
• W2419258853 cites W4238410788 @default.
• W2419258853 doi "https://doi.org/10.1016/j.oregeorev.2016.05.028" @default.
• W2419258853 hasPublicationYear "2016" @default.
• W2419258853 type Work @default.
• W2419258853 sameAs 2419258853 @default.
• W2419258853 citedByCount "19" @default.
• W2419258853 countsByYear W24192588532016 @default.
• W2419258853 countsByYear W24192588532017 @default.
• W2419258853 countsByYear W24192588532018 @default.
• W2419258853 countsByYear W24192588532019 @default.
• W2419258853 countsByYear W24192588532020 @default.
• W2419258853 countsByYear W24192588532021 @default.
• W2419258853 countsByYear W24192588532022 @default.
• W2419258853 countsByYear W24192588532023 @default.
• W2419258853 crossrefType "journal-article" @default.
• W2419258853 hasAuthorship W2419258853A5011065438 @default.
• W2419258853 hasAuthorship W2419258853A5029695428 @default.
• W2419258853 hasAuthorship W2419258853A5062195279 @default.
• W2419258853 hasAuthorship W2419258853A5066742396 @default.
• W2419258853 hasAuthorship W2419258853A5069687620 @default.
• W2419258853 hasAuthorship W2419258853A5071418521 @default.
• W2419258853 hasAuthorship W2419258853A5090034308 @default.
• W2419258853 hasConcept C127313418 @default.
• W2419258853 hasConcept C151730666 @default.
• W2419258853 hasConcept C17409809 @default.
• W2419258853 hasConcept C199289684 @default.
• W2419258853 hasConcept C2777746296 @default.
• W2419258853 hasConcept C2777781897 @default.
• W2419258853 hasConcept C2779181077 @default.
• W2419258853 hasConcept C2779870107 @default.
• W2419258853 hasConcept C2780375929 @default.
• W2419258853 hasConcept C34682378 @default.
• W2419258853 hasConcept C57830525 @default.
• W2419258853 hasConceptScore W2419258853C127313418 @default.
• W2419258853 hasConceptScore W2419258853C151730666 @default.
• W2419258853 hasConceptScore W2419258853C17409809 @default.
• W2419258853 hasConceptScore W2419258853C199289684 @default.
• W2419258853 hasConceptScore W2419258853C2777746296 @default.

• next