The late Tonian Zhaunkar granite complex of the Ulutau sialic massif, Central Kazakhstan

A. A. Tretyakov; K. E. Degtyarev; E. B. Salnikova; K. N. Shatagin; A. B. Kotov; I. V. Anisimova; Yu. V. Plotkina

doi:10.1134/S1028334X17040225

The late Tonian Zhaunkar granite complex of the Ulutau sialic massif, Central Kazakhstan

Autores: Tretyakov A.A.¹, Degtyarev K.E.¹, Salnikova E.B.², Shatagin K.N.³, Kotov A.B.², Anisimova I.V.², Plotkina Y.V.²
Afiliações:
1. Geological Institute
2. Institute of Precambrian Geology and Geochronology
3. Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Edição: Volume 473, Nº 2 (2017)
Páginas: 411-415
Seção: Geology
URL: https://ogarev-online.ru/1028-334X/article/view/189621
DOI: https://doi.org/10.1134/S1028334X17040225
ID: 189621

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The crystallization age of Zhaunkar granites (829 ± 10 Ma) was determined by U–Pb zircon dating. Taking into account the data obtained earlier on the granite age (791 ± 7 Ma) in the Aktas Complex and the syenite age (673 ± 2 Ma) in the Karsakpai Complex, the Ulutau sialic massif is assumed to be composed of three igneous complexes formed during the Tonian–Cryogenian periods of the Neoproterozoic.