Late Vendian Complexes in the Structure of Metamorphic Basement of the Fore Range Zone, Greater Caucasus


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The paper presents new data on the composition, age, and relationships (with host and overlying deposits) of intrusive rocks in the basement of the Fore Range zone (Greater Caucasus), in the Malaya Laba River Basin. The evolutionary features of intrusive units located within the Blyb metamorphic complex are described. It is shown for the first time that the lower levels of this complex are, in a structural sense, outcrops of the Late Vendian basement. The basement is composed of the Balkan Formation and a massif of quartz metadiorites that intrudes it; for the rocks of this massif, ages ranging from 549 ± 7.4 to 574.1 ± 6.7 Ma are obtained for three U–Pb datings by the SHRIMP-II method. The Herzyinan magmatic event is represented by a group of granodiorite intrusions penetrating the Blyb complex on a series of faults extending along its boundary with the Main Range zone. The obtained estimate for the U–Pb age of one of the intrusions (319 ± 3.8 Ma) corresponds to the end of the Serpukhovian stage of the Early Carboniferous.

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V. Kamzolkin

Schmidt Institute of Physics of the Earth

编辑信件的主要联系方式.
Email: vkamzolkin@gmail.com
俄罗斯联邦, Moscow, 123242

A. Latyshev

Schmidt Institute of Physics of the Earth; Department of Geology

Email: vkamzolkin@gmail.com
俄罗斯联邦, Moscow, 123242; Moscow, 119991

Yu. Vidyapin

Schmidt Institute of Physics of the Earth

Email: vkamzolkin@gmail.com
俄罗斯联邦, Moscow, 123242

M. Somin

Schmidt Institute of Physics of the Earth

Email: vkamzolkin@gmail.com
俄罗斯联邦, Moscow, 123242

A. Smul’skaya

Schmidt Institute of Physics of the Earth

Email: vkamzolkin@gmail.com
俄罗斯联邦, Moscow, 123242

S. Ivanov

Schmidt Institute of Physics of the Earth

Email: vkamzolkin@gmail.com
俄罗斯联邦, Moscow, 123242

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