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 |
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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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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.</description><identifier>ISSN: 1028-334X</identifier><identifier>EISSN: 1531-8354</identifier><identifier>DOI: 10.1134/S1028334X22601043</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Belts ; Cratons ; Earth and Environmental Science ; Earth Sciences ; Feldspars ; Geochronology ; Geology ; Lead ; Mica ; Mineralogical research ; Plagioclase</subject><ispartof>Doklady earth sciences, 2022-12, Vol.507 (2), p.987-993</ispartof><rights>Pleiades Publishing, Ltd. 2022. ISSN 1028-334X, Doklady Earth Sciences, 2022, Vol. 507, Part 2, pp. 987–993. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2022, published in Doklady Rossiiskoi Akademii Nauk. 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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.</description><subject>Belts</subject><subject>Cratons</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Feldspars</subject><subject>Geochronology</subject><subject>Geology</subject><subject>Lead</subject><subject>Mica</subject><subject>Mineralogical research</subject><subject>Plagioclase</subject><issn>1028-334X</issn><issn>1531-8354</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><recordid>eNp1kM1KAzEUhYMoWKsP4C7gRhdT8zc_cVdbq4VWC21BdDGkyZ06pTNTkyniznfwDX0SM1RwIZJFcs89383lIHRKSYdSLi6nlLCEc_HIWEQoEXwPtWjIaZDwUOz7t28HTf8QHTm3IkQIEcoWep69AB5UtlB1XpW4uwRcZXgCy0aowTVV7S1jVSg8zrXC17Cur_A9vOH518fnZIHPh_1gNhxPL3Bf1Qr7KU-51VXpjtFBptYOTn7uNpoPbma9u2D0cDvsdUeB5iSuA4gNCMZklCgtvKKVVIkJF7FZgMmMJIaaLIREUgkQas50ZKg2oZSZoIxGvI3OdnM3tnrdgqvTVbW1pf8yZXEUERkKyr2rs3Mt1RrSvMyq2irtj4Ei9-tClnu9G3PuY-OeaCO6A7StnLOQpRubF8q-p5SkTejpn9A9w3aM895yCfZ3lf-hbzyPgT0</recordid><startdate>20221201</startdate><enddate>20221201</enddate><creator>Tkachev, A. 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V.</au><au>Plotkina, Yu.V.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The Formation Age of Pegmatites of the Mama Mica Belt: New U–Pb (ID-TIMS) Data on Zircons</atitle><jtitle>Doklady earth sciences</jtitle><stitle>Dokl. Earth Sc</stitle><date>2022-12-01</date><risdate>2022</risdate><volume>507</volume><issue>2</issue><spage>987</spage><epage>993</epage><pages>987-993</pages><issn>1028-334X</issn><eissn>1531-8354</eissn><abstract>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. 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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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