The Formation Age of Pegmatites of the Mama Mica Belt: New U–Pb (ID-TIMS) Data on Zircons

New geochronological (U–Pb ID-TIMS) data on zircons from pegmatites of the Mama mica belt in the Baikal Highlands are presented. The ages obtained for the plagioclase pegmatites (388 ± 2 and 389 ± 2 Ma, Mochikit deposit) and two-feldspar pegmatites (333 ± 1 and 332 ± 3 Ma, Slyudyanka deposit) demons...

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Veröffentlicht in:Doklady earth sciences 2022-12, Vol.507 (2), p.987-993
Hauptverfasser: Tkachev, A. V., Sal’nikova, E. B., Rytsk, E. Yu, Kotov, A. B., Ivanova, A. A., Tolmacheva, E. V., Plotkina, Yu.V.
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container_issue 2
container_start_page 987
container_title Doklady earth sciences
container_volume 507
creator Tkachev, A. V.
Sal’nikova, E. B.
Rytsk, E. Yu
Kotov, A. B.
Ivanova, A. A.
Tolmacheva, E. V.
Plotkina, Yu.V.
description New geochronological (U–Pb ID-TIMS) data on zircons from pegmatites of the Mama mica belt in the Baikal Highlands are presented. The ages obtained for the plagioclase pegmatites (388 ± 2 and 389 ± 2 Ma, Mochikit deposit) and two-feldspar pegmatites (333 ± 1 and 332 ± 3 Ma, Slyudyanka deposit) demonstrate a significant age gap (50–60 Ma) between them. Based on the entire set of geological and new geochronological data available, it is proposed to divide the Mama complex, to which they were previously assigned, into two separate granitoid complexes.
doi_str_mv 10.1134/S1028334X22601043
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subjects Belts
Cratons
Earth and Environmental Science
Earth Sciences
Feldspars
Geochronology
Geology
Lead
Mica
Mineralogical research
Plagioclase
title The Formation Age of Pegmatites of the Mama Mica Belt: New U–Pb (ID-TIMS) Data on Zircons
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