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


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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.

作者简介

A. Tretyakov

Geological Institute

Email: degtkir@ginras.ru
俄罗斯联邦, Pyzhevsky per. 7, Moscow, 119017

K. Degtyarev

Geological Institute

编辑信件的主要联系方式.
Email: degtkir@ginras.ru
俄罗斯联邦, Pyzhevsky per. 7, Moscow, 119017

E. Salnikova

Institute of Precambrian Geology and Geochronology

Email: degtkir@ginras.ru
俄罗斯联邦, nab. Makarova 2, St. Petersburg, 199034

K. Shatagin

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

Email: degtkir@ginras.ru
俄罗斯联邦, Staromonetny per. 7, Moscow, 119117

A. Kotov

Institute of Precambrian Geology and Geochronology

Email: degtkir@ginras.ru
俄罗斯联邦, nab. Makarova 2, St. Petersburg, 199034

I. Anisimova

Institute of Precambrian Geology and Geochronology

Email: degtkir@ginras.ru
俄罗斯联邦, nab. Makarova 2, St. Petersburg, 199034

Yu. Plotkina

Institute of Precambrian Geology and Geochronology

Email: degtkir@ginras.ru
俄罗斯联邦, nab. Makarova 2, St. Petersburg, 199034

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