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Granitic magma evolution to magmatic-hydrothermal processes vital to the generation of HREEs ion-adsorption deposits: Constraints from zircon texture, U-Pb geochronology, and geochemistry

dc.contributor.authorXu, Zhao
dc.contributor.authorLi, Ning-Bo
dc.contributor.authorHuizenga, Jan Marten
dc.contributor.authorYang, Yu-Yuang
dc.contributor.authorYan, Shuang
dc.contributor.authorYang, Wu-bing
dc.contributor.authorNiu, He-Cai
dc.date.accessioned2022-06-16T10:39:57Z
dc.date.available2022-06-16T10:39:57Z
dc.date.created2022-05-14T18:24:56Z
dc.date.issued2022
dc.identifier.issn0169-1368
dc.identifier.urihttps://hdl.handle.net/11250/2999039
dc.language.isoeng
dc.titleGranitic magma evolution to magmatic-hydrothermal processes vital to the generation of HREEs ion-adsorption deposits: Constraints from zircon texture, U-Pb geochronology, and geochemistry
dc.title.alternativeGranitic magma evolution to magmatic-hydrothermal processes vital to the generation of HREEs ion-adsorption deposits: Constraints from zircon texture, U-Pb geochronology, and geochemistry
dc.typePeer reviewed
dc.typeJournal article
dc.description.versionpublishedVersion
dc.source.journalOre Geology Reviews
dc.identifier.doi10.1016/j.oregeorev.2022.104931
dc.identifier.cristin2024618
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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