Western structural closing of the Pripyat–Dneprov–Donetsk aulacogen-Reference-Cited by-同舟云学术

Western structural closing of the Pripyat–Dneprov–Donetsk aulacogen

Published:2022-11-03 Issue:5 Volume:66 Page:533-543
ISSN:2524-2431
Container-title:Doklady of the National Academy of Sciences of Belarus
language:
Short-container-title:Dokl. Akad. nauk

Author:

Aizberg R. E.¹,Gribik Ya. G.¹,Garetsky R. G.¹

Affiliation:

1. Institute of Nature Management of the National Academy of Sciences of Belarus

Abstract

In segmented paleorift systems such as the Pripyat–Dnieper–Donetsk aulacogen, which penetrate deep into the continent from the side of the paleoocean margin and most often close here, each segment represents an autonomous structure of the lithosphere. The presented article shows that the tectonic position of the Pripyat paleorift as the western closing segment of the indicated aulacogen was due to a change in the intensity of syn-rift and plate-tectonic processes in the extended rift system from east to west. In the band of the Paleoproterozoic Fenno-Sarmatian collision, the Central Belarusian suture zone of the Central Russian transpression belt isolated by S. V. Bogdanova in 2018 was a blocking transverse barrier to relative development of Hercynian synrift processes in the western direction.

Publisher

Publishing House Belorusskaya Nauka

Subject

General Medicine

Reference13 articles.

1. Aizberg R. E. Segmentation of the Pripyat–Dnieper–Donetsk aulacogen. Doklady Natsional’noi akademii nauk Belarusi = Doklady of the National Academy of Sciences of Belarus, 2016, vol. 60, no. 6, рр. 111–116 (in Russian).

2. Shchipansky А. А., Bogdanova S. V. The Sarmatian crustal segment: Precambrian correlation between the Voronezh Massif and the Ukrainian Shield across the Dniepr–Donets Aulacogen. Tectonophysics, 1996, vol. 268, no. 1–4, pp. 109–125. https://doi. org/10.1016/s0040-1951(96)00227-2

3. Naidenkov I. V. Smolevichy–Drogichin zone – a suture type structure in the crystalline basement of Belarus. Litasfera [Lithosphere], 1998, no. 8, рр. 83–91 (in Russian).

4. Garetsky R. G. Model of the structure of the lithosphere along the Central Belarusian geotransect. Doklady Natsional’noi akademii nauk Belarusi = Doklady of the National Academy of Sciences of Belarus, 1999, vol. 43, no. 2, рр. 87–89 (in Russian).

5. Bogdanova S. Segments of the East European Craton. EUROPROBE in Jablonna 1991. Warszawa, 1993, рр. 33–38.