Late Vendian postcollisional leucogranites of Yenisei Ridge

The Late Vendian (540–550 Ma) U–Pb zircon age of postcollisional granitoids in the Osinovka Massif was obtained for the first time. The Osinovka Massif is located in rocks of the island-arc complex of the Isakovka Terrane, in the northwestern part of the Sayany–Yenisei accretion belt. These events s...

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Published in:Doklady earth sciences 2017-06, Vol.474 (2), p.674-679
Main Authors: Nozhkin, A. D., Likhanov, I. I., Reverdatto, V. V., Bayanova, T. B., Zinoviev, S. V., Kozlov, P. S., Popov, N. V., Dmitrieva, N. V.
Format: Article
Language:English
Subjects:
Accretion
Composition
Continental crust
Cratons
Deposition
Dimensions
Earth and Environmental Science
Earth Sciences
Fragmentation
Fragments
Geochemistry
Geochronometry
Geological time
Granite
History
Island arcs
Isotopes
Magma
Oceanic crust
Radiometric dating
Rock
Rocks
Thrust
Zircon
Zirconium
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cited_by cdi_FETCH-LOGICAL-a378t-3655a904da69190a5061f98e38697ca80af6c2724306eed5701889c770358a53
cites cdi_FETCH-LOGICAL-a378t-3655a904da69190a5061f98e38697ca80af6c2724306eed5701889c770358a53
container_end_page 679
container_issue 2
container_start_page 674
container_title Doklady earth sciences
container_volume 474
creator Nozhkin, A. D.
Likhanov, I. I.
Reverdatto, V. V.
Bayanova, T. B.
Zinoviev, S. V.
Kozlov, P. S.
Popov, N. V.
Dmitrieva, N. V.
description The Late Vendian (540–550 Ma) U–Pb zircon age of postcollisional granitoids in the Osinovka Massif was obtained for the first time. The Osinovka Massif is located in rocks of the island-arc complex of the Isakovka Terrane, in the northwestern part of the Sayany–Yenisei accretion belt. These events stand for the final stage of the Neoproterozoic history of the Yenisei Ridge, related to the completing accretion of the oceanic crust fragments and the beginning of the Caledonian orogenesis. The petrogeochemical composition and the Sm–Nd isotopic characteristics support the fact that the granitoid melt originated from a highly differentiated continental crust of the southwestern margin of the Siberian Craton. Hence, the granite-bearing Late Riphean island-arc complexes were thrust over the craton margin at a distance considerably exceeding the dimensions of the Osinovka Massif.
doi_str_mv 10.1134/S1028334X17060125
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subjects Accretion
Composition
Continental crust
Cratons
Deposition
Dimensions
Earth and Environmental Science
Earth Sciences
Fragmentation
Fragments
Geochemistry
Geochronometry
Geological time
Granite
History
Island arcs
Isotopes
Magma
Oceanic crust
Radiometric dating
Rock
Rocks
Thrust
Zircon
Zirconium
title Late Vendian postcollisional leucogranites of Yenisei Ridge
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