Plume magmatism in the northeastern part of the Altai–Sayan region: Stages, source compositions, and geodynamics (exemplified by the Minusinsk Depression)


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The results of geochronological (U–Pb, Ar–Ar), geochemical, and isotopic (Sr, Nd) studies of the Ordovician and Devonian mafic volcanic–subvolcanic rock associations of the Minusinsk Depression are presented. The obtained ages of magmatic associations and the basite composition, considering previous studies, witness to the impact of two mantle plumes different in age (Late Cambrian–Ordovician and Devonian) on suprasubduction rock complexes in active continental margin settings.

作者简介

A. Vorontsov

Vinogradov Institute of Geochemistry, Siberian Branch; Irkutsk State University

编辑信件的主要联系方式.
Email: voron@igc.irk.ru
俄罗斯联邦, Irkutsk, 664033; Irkutsk

O. Perfilova

Siberian Federal University

Email: voron@igc.irk.ru
俄罗斯联邦, Krasnoyarsk

M. Buslov

Sobolev Institute of Geology and Mineralogy, Siberian Branch; Novosibirsk State University

Email: voron@igc.irk.ru
俄罗斯联邦, Novosibirsk, 630090; Novosibirsk

A. Travin

Sobolev Institute of Geology and Mineralogy, Siberian Branch; Novosibirsk State University

Email: voron@igc.irk.ru
俄罗斯联邦, Novosibirsk, 630090; Novosibirsk

M. Makhlaev

Siberian Federal University

Email: voron@igc.irk.ru
俄罗斯联邦, Krasnoyarsk

S. Dril

Vinogradov Institute of Geochemistry, Siberian Branch

Email: voron@igc.irk.ru
俄罗斯联邦, Irkutsk, 664033

Ya. Katraevskaya

Irkutsk State University

Email: voron@igc.irk.ru
俄罗斯联邦, Irkutsk


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