FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2891574105> ?p ?o ?g. }

• W2891574105 endingPage "34" @default.
• W2891574105 startingPage "28" @default.
• W2891574105 abstract "Trace elements in igneous zircon crystals are variable within single crystals or amongst populations of crystals and are particularly sensitive to changes in melt composition. In this study, we present zircon trace element data from both volcanic and plutonic rocks of the Yandangshan caldera complex from SEChina. The erupted rhyolitic rocks are interpreted to represent the most differentiated magma, whereas the intruded porphyritic quartz syenites are thought to be representative of the residual crystal mush. The zircon crystals of both lithologies are subdivided into two types based on their internal structures: type A with a distinct oscillatory growth zoning and type B crystals are bright in cathodoluminescence (CL-bright). Type B zircon occurs as rims of type A zircon or as individual grains. Compared to type A, type B zircons commonly show lower Hf, U, Th and Y concentrations and higher Ti and Zr/Hf and Eu/Eu* ratios. The zircon trace element compositions of the volcanic samples generally overlap those of the intracaldera porphyritic quartz syenite and mafic microgranular enclaves that contain both type A and type B zircons. Despite a general overlap, zircon grains from the volcanic rocks show relatively higher Hf contents and Y/Dy ratios, lower Ti contents and Th/U ratios and larger negative Eu anomalies than the plutonic samples. We suggest that the inter- and intragrain compositional variability of zircon crystals can be used to track the evolution of magmatic systems. We show that in our case, the volcanic and plutonic rocks crystallized continuously during the magmatic evolution in a common magma system and that the magmas of these rocks may be linked by fractional crystallization. Furthermore, the type B zircon grains are inferred to have crystalized in relatively hot and less evolved magma indicating a magma recharge event. Consequently, the geochemical variability of igneous zircon crystals can be used to infer on the magmatic evolution of single volcanic system which may also be applicable in other geodynamic environments." @default.
• W2891574105 created "2018-09-27" @default.
• W2891574105 creator A5046919861 @default.
• W2891574105 creator A5048602354 @default.
• W2891574105 creator A5064629858 @default.
• W2891574105 creator A5069054353 @default.
• W2891574105 date "2018-11-01" @default.
• W2891574105 modified "2023-10-17" @default.
• W2891574105 title "Zircon trace element constrains on the link between volcanism and plutonism in SE China" @default.
• W2891574105 cites W1525258218 @default.
• W2891574105 cites W1948519936 @default.
• W2891574105 cites W1966237762 @default.
• W2891574105 cites W1969375798 @default.
• W2891574105 cites W1977392315 @default.
• W2891574105 cites W1984025404 @default.
• W2891574105 cites W1997710040 @default.
• W2891574105 cites W1998302453 @default.
• W2891574105 cites W2012845152 @default.
• W2891574105 cites W2015239493 @default.
• W2891574105 cites W2016998014 @default.
• W2891574105 cites W2027819494 @default.
• W2891574105 cites W2040659190 @default.
• W2891574105 cites W2048084357 @default.
• W2891574105 cites W2052439962 @default.
• W2891574105 cites W2054176003 @default.
• W2891574105 cites W2054653182 @default.
• W2891574105 cites W2065291589 @default.
• W2891574105 cites W2068099788 @default.
• W2891574105 cites W2073005317 @default.
• W2891574105 cites W2074699374 @default.
• W2891574105 cites W2076724145 @default.
• W2891574105 cites W2077932190 @default.
• W2891574105 cites W2086557360 @default.
• W2891574105 cites W2087470623 @default.
• W2891574105 cites W2090695609 @default.
• W2891574105 cites W2093369526 @default.
• W2891574105 cites W2094373534 @default.
• W2891574105 cites W2118670133 @default.
• W2891574105 cites W2123698291 @default.
• W2891574105 cites W2130612399 @default.
• W2891574105 cites W2157508130 @default.
• W2891574105 cites W2161205090 @default.
• W2891574105 cites W2162359721 @default.
• W2891574105 cites W2163661859 @default.
• W2891574105 cites W2164983848 @default.
• W2891574105 cites W2175880406 @default.
• W2891574105 cites W2310440499 @default.
• W2891574105 cites W2321976203 @default.
• W2891574105 cites W2460503747 @default.
• W2891574105 cites W2544640391 @default.
• W2891574105 cites W2583986954 @default.
• W2891574105 cites W2603981417 @default.
• W2891574105 cites W2610727812 @default.
• W2891574105 cites W2772064553 @default.
• W2891574105 cites W2773863138 @default.
• W2891574105 cites W2792248697 @default.
• W2891574105 doi "https://doi.org/10.1016/j.lithos.2018.08.040" @default.
• W2891574105 hasPublicationYear "2018" @default.
• W2891574105 type Work @default.
• W2891574105 sameAs 2891574105 @default.
• W2891574105 citedByCount "33" @default.
• W2891574105 countsByYear W28915741052019 @default.
• W2891574105 countsByYear W28915741052020 @default.
• W2891574105 countsByYear W28915741052021 @default.
• W2891574105 countsByYear W28915741052022 @default.
• W2891574105 countsByYear W28915741052023 @default.
• W2891574105 crossrefType "journal-article" @default.
• W2891574105 hasAuthorship W2891574105A5046919861 @default.
• W2891574105 hasAuthorship W2891574105A5048602354 @default.
• W2891574105 hasAuthorship W2891574105A5064629858 @default.
• W2891574105 hasAuthorship W2891574105A5069054353 @default.
• W2891574105 hasConcept C104962623 @default.
• W2891574105 hasConcept C120806208 @default.
• W2891574105 hasConcept C127313418 @default.
• W2891574105 hasConcept C151730666 @default.
• W2891574105 hasConcept C167236342 @default.
• W2891574105 hasConcept C167284885 @default.
• W2891574105 hasConcept C17409809 @default.
• W2891574105 hasConcept C183222429 @default.
• W2891574105 hasConcept C192241223 @default.
• W2891574105 hasConcept C193429443 @default.
• W2891574105 hasConcept C25822816 @default.
• W2891574105 hasConcept C2778849375 @default.
• W2891574105 hasConcept C2779670319 @default.
• W2891574105 hasConcept C2779870107 @default.
• W2891574105 hasConcept C34122518 @default.
• W2891574105 hasConcept C34682378 @default.
• W2891574105 hasConcept C42787717 @default.
• W2891574105 hasConcept C5900021 @default.
• W2891574105 hasConcept C77928131 @default.
• W2891574105 hasConceptScore W2891574105C104962623 @default.
• W2891574105 hasConceptScore W2891574105C120806208 @default.
• W2891574105 hasConceptScore W2891574105C127313418 @default.
• W2891574105 hasConceptScore W2891574105C151730666 @default.
• W2891574105 hasConceptScore W2891574105C167236342 @default.
• W2891574105 hasConceptScore W2891574105C167284885 @default.
• W2891574105 hasConceptScore W2891574105C17409809 @default.
• W2891574105 hasConceptScore W2891574105C183222429 @default.

• next