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


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Abstract

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.

About the authors

A. A. Tretyakov

Geological Institute

Email: degtkir@ginras.ru
Russian Federation, Pyzhevsky per. 7, Moscow, 119017

K. E. Degtyarev

Geological Institute

Author for correspondence.
Email: degtkir@ginras.ru
Russian Federation, Pyzhevsky per. 7, Moscow, 119017

E. B. Salnikova

Institute of Precambrian Geology and Geochronology

Email: degtkir@ginras.ru
Russian Federation, nab. Makarova 2, St. Petersburg, 199034

K. N. Shatagin

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

Email: degtkir@ginras.ru
Russian Federation, Staromonetny per. 7, Moscow, 119117

A. B. Kotov

Institute of Precambrian Geology and Geochronology

Email: degtkir@ginras.ru
Russian Federation, nab. Makarova 2, St. Petersburg, 199034

I. V. Anisimova

Institute of Precambrian Geology and Geochronology

Email: degtkir@ginras.ru
Russian Federation, nab. Makarova 2, St. Petersburg, 199034

Yu. V. Plotkina

Institute of Precambrian Geology and Geochronology

Email: degtkir@ginras.ru
Russian Federation, nab. Makarova 2, St. Petersburg, 199034


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