First Age and Geochemical Data on Zircon from Riebeckite Granites of the Verkhnee Espe Rare Earth–Rare Metal Deposit, East Kazakhstan

This paper is dedicated to the isotope-geochemical study of zircon from riebeckite granites of the Verkhnee Espe rare earth-rare metal deposit and the specification of its U–Pb age. Zircon from the Verkhnee Espe massif is peculiar in the high content of non-formula elements (up to 43000 ppm REE, up...

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Veröffentlicht in:Geochemistry international 2022, Vol.60 (1), p.1-15
Hauptverfasser: Levashova, E. V., Skublov, S. G., Oitseva, T. A., Dyachkov, B. A., Li, X.-H., Li, Q.-L., Shatova, N. V., Shatov, V. V.
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container_title Geochemistry international
container_volume 60
creator Levashova, E. V.
Skublov, S. G.
Oitseva, T. A.
Dyachkov, B. A.
Li, X.-H.
Li, Q.-L.
Shatova, N. V.
Shatov, V. V.
description This paper is dedicated to the isotope-geochemical study of zircon from riebeckite granites of the Verkhnee Espe rare earth-rare metal deposit and the specification of its U–Pb age. Zircon from the Verkhnee Espe massif is peculiar in the high content of non-formula elements (up to 43000 ppm REE, up to 22000 Y, and others) and demonstrates a clearly expressed heterogeneous structure. The central and rim zones of the zircon show a “magmatic” rare-earth element (REE) distribution. The intermediate zones are characterized by a flattening of the REE patterns and an anomalous enrichment in REE, Y, Nb, and Ca. This compositional feature of the zircon may be caused by impact of fluid-saturated granite melts enriched in incompatible trace elements. The δ 18 О values in the zircon are 5.83–7.16‰, which generally corresponds to zircon formed from granitoid melts. The age of zircon from the Verkhnee Espe rare earth–rare metal deposit is 283 ± 3 Ma, which indicates that there is no significant age gap between granite crystallization, on the one hand, and metasomatic processes and ore generation, on the other.
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V. ; Skublov, S. G. ; Oitseva, T. A. ; Dyachkov, B. A. ; Li, X.-H. ; Li, Q.-L. ; Shatova, N. V. ; Shatov, V. V.</creator><creatorcontrib>Levashova, E. V. ; Skublov, S. G. ; Oitseva, T. A. ; Dyachkov, B. A. ; Li, X.-H. ; Li, Q.-L. ; Shatova, N. V. ; Shatov, V. V.</creatorcontrib><description>This paper is dedicated to the isotope-geochemical study of zircon from riebeckite granites of the Verkhnee Espe rare earth-rare metal deposit and the specification of its U–Pb age. Zircon from the Verkhnee Espe massif is peculiar in the high content of non-formula elements (up to 43000 ppm REE, up to 22000 Y, and others) and demonstrates a clearly expressed heterogeneous structure. The central and rim zones of the zircon show a “magmatic” rare-earth element (REE) distribution. The intermediate zones are characterized by a flattening of the REE patterns and an anomalous enrichment in REE, Y, Nb, and Ca. 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The central and rim zones of the zircon show a “magmatic” rare-earth element (REE) distribution. The intermediate zones are characterized by a flattening of the REE patterns and an anomalous enrichment in REE, Y, Nb, and Ca. This compositional feature of the zircon may be caused by impact of fluid-saturated granite melts enriched in incompatible trace elements. The δ 18 О values in the zircon are 5.83–7.16‰, which generally corresponds to zircon formed from granitoid melts. 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subjects Age
Asbestos
Crystallization
Earth
Earth and Environmental Science
Earth Sciences
Geochemistry
Granite
Heavy metals
Heterogeneous structure
Isotopes
Massifs
Melts
Radiometric dating
Rare earth elements
Rare earth metals
Trace elements
Yttrium
Zircon
title First Age and Geochemical Data on Zircon from Riebeckite Granites of the Verkhnee Espe Rare Earth–Rare Metal Deposit, East Kazakhstan
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