Dmitrii P. Gladkochub

Institute of the Earth’s Crust

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ВБ

В. Б. Хубанов

Siberian Branch of the Russian Academy of Sciences

ТV

Т. V. Donskaya

Institute of the Earth’s Crust

Z. L. Motova

Institute of the Earth’s Crust

Tao Wang

Huaiyin Normal University

Adam Abersteiner

University of Helsinki

V. D. Shcherbakov

Lomonosov Moscow State University

Alexander V. Sizov

Geological Institute

Vadim S. Kamenetsky

Institute of Experimental Mineralogy

ВМ

В. М. Саватенков

Institute of Precambrian Geology and Geochronology

A. M. Pasenko

Schmidt Institute of Physics of the Earth

Cooperative Institutions

Russian Academy of Sciences

Institute of the Earth’s Crust

University of Tasmania

Geological Institute

Chinese Academy of Sciences

St Petersburg University

University of Adelaide

Institute of Volcanology and Seismology

Far Eastern Branch of the Russian Academy of Sciences

Lomonosov Moscow State University

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Geodynamic Significance of the Mesoproterozoic Magmatism of the Udzha Paleo-Rift (Northern Siberian Craton) Based on U-Pb Geochronology and Paleomagnetic Data

Minerals (2018)

С. В. Малышев A. M. Pasenko А. В. Иванов Dmitrii P. Gladkochub В. М. Саватенков

The emplacement age of the Great Udzha Dyke (northern Siberian Craton) was determined by the U-Pb dating of apatite using laser ablation inductively coupled plasma mass spectrometry (LA-ICPMS). This produced an age of 1386 ± 30 Ma. This dyke along with two other adjacent intrusions, which cross-cut the sedimentary units of the Udzha paleo-rift, were subjected to paleomagnetic investigation. The paleomagnetic poles for the Udzha paleo-rift intrusions are consistent with previous results published for the Chieress dyke in the Anabar shield of the Siberian Craton (1384 ± 2 Ma). Our results suggest that there was a period of intense volcanism in the northern Siberian Craton, as well as allow us to reconstruct the apparent migration of the Siberian Craton during the Mesoproterozoic.

Geochronology

Rodinia

10.3390/min8120555

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Citations (17)

First China-Russia International Meeting on the Central Asian Orogenic Belt and IGCP-592 Workshop

Episodes (2016)

Inna Safonova Tao Wang Bei Lei Xu Dmitrii P. Gladkochub Ying Tong

of the tectonic evolution of the southern CAOB occupied the first place of five research fronts in the earth sciences identified by the publisher Elsevier Ltd.The CAOB extends across Russia, China, Kazakhstan, Kyrgyzstan, Uzbekistan, Tajikistan and Mongolia.Due to its huge size, extensive and intensive international cooperation researches and, particularly, across-border comparative studies are necessary to improve our understanding of its long and complex evolution.Consequently, CAOB geologists all agree that it is necessary to build a platform of communication between researchers from Russia, China and other countries to exchange new data and ideas and to discuss and plan future cooperative projects.

Central Asia

10.18814/epiiugs/2016/v39i3/008

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Citations (1)

Cambrian/Ordovician boundary as a milestone in the sedimentation history of the southern Siberian craton: Evidence from U-Pb dating of detrital zircons

Journal of Asian Earth Sciences X (2022)

Dmitrii P. Gladkochub Z. L. Motova Т. V. Donskaya В. Б. Хубанов Alexander V. Sizov

Felsic

Laurentia

10.1016/j.jaesx.2022.100107

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Citations (9)