R. G. Garetsky

Institute of Nature Management

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РЕ

Р. Е. Айзберг

Institute of Nature Management

Ya. G. Gribik

National Academy of Sciences of Belarus

Roland Gorbatschev

Lund University

Svetlana Bogdanova

Stavropol State Agrarian University

Hans Thybo

Chinese Academy of Geological Sciences

R. P. Litvinovskaya

National Academy of Sciences of Belarus

АК

А. К. Карабанов

National Academy of Sciences of Belarus

A. Guterch

Institute of Geophysics

V. Omelchenko

National Academy of Sciences of Ukraine

Dmytro Lysynchuk

National Academy of Sciences of Ukraine

Cooperative Institutions

National Academy of Sciences of Belarus

National Academy of Sciences of Ukraine

Institute of Bioorganic Chemistry

Palladin Institute of Biochemistry

Institute of Nature Management

Institute of Geophysics

Polish Academy of Sciences

Russian Academy of Sciences

University of Warsaw

Uppsala University

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EUROPE | East European Craton

Elsevier eBooks (2005)

Svetlana Bogdanova Roland Gorbatschev R. G. Garetsky

10.1016/b0-12-369396-9/00426-3

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Citations (40)

Western structural closing of the Pripyat–Dneprov–Donetsk aulacogen

Doklady of the National Academy of Sciences of Belarus (2022)

Р. Е. Айзберг Ya. G. Gribik R. G. Garetsky

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.

10.29235/1561-8323-2022-66-5-533-543

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Lithospheric structure along wide-angle seismic profile GEORIFT 2013 in Pripyat–Dnieper–Donets Basin (Belarus and Ukraine)

Geophysical Journal International (2017)

V. I. Starostenko Tomasz Janik Tamara Yegorova Wojciech Czuba Piotr Środa

The GEORIFT 2013 (GR'13) WARR (wide-angle reflection and refraction) experiment was carried out in 2013 in the territory of Belarus and Ukraine with broad international co-operation. The aim of the work is to study basin architecture and deep structure of the Pripyat–Dnieper–Donets Basin (PDDB), which is the deepest and best studied Palaeozoic rift basin in Europe. The PDDB is located in the southern part of the East European Craton (EEC) and crosses Sarmatia—one of the three segments of the EEC. The PDDB was formed by Late Devonian rifting associated with domal basement uplift and magmatism. The GR'13 extends in NW–SE direction along the PDDB strike and crosses the Pripyat Trough (PT) and Dnieper Graben (DG) separated by the Bragin Uplift (BU) of the basement. The field acquisition along the GR'13 (of 670 km total length) involved 14 shots and recorders deployed every ∼2.2 km for several shot points. The good quality of the data, with first arrivals visible up to 670 km for several shot points, allowed for construction of a velocity model extending to 80 km depth using ray-tracing modelling. The thickness of the sediments (Vp < 6.0 km s−1) varies from 1–4 km in the PT, to ∼5 km in the NW part of the DG, to 10–13 km in the SE part of the profile. Below the DG, at ∼330–530 km distance, we observed an upwarping of the lower crust (with Vp of ∼7.1 km s−1) to ∼25 km depth that represents a rift pillow or mantle underplate. The Moho shallows southeastwards from ∼47 km in the PT to 40–38 km in the DG with mantle velocities of 8.35 and ∼8.25 km s−1 in the PT and DG, respectively. A near-horizontal mantle discontinuity was found beneath BU (a transition zone from the PT to the DG) at the depth of 50–47 km. It dips to the depth of ∼60 km at distances of 360–405 km, similar to the intersecting EUROBRIDGE'97 profile. The crust and upper mantle structure on the GR'13 may reflect varying intensity of rifting in the PDDB from a passive stage in the PT to active rifting in the DG. The absence of Moho uplift and relatively thick crystalline crust under the PT is explained by its tectonic position as a closing unit of the PDDB, with a gradual attenuation of rifting from the southeast to the northwest. The most active stage of rifting is evidenced in the DG by a shallower Moho and by a presence of a rift pillow caused by mafic and ultramafic intrusions during the active phase. The junction of the PT and the DG (the BU) locates just at its intersection with the NS regional tectonic zone Odessa-Gomel. Most likely, the 'blocking' effect of this zone did not allow for further propagation of active rifting to the NW.

Devonian

Basement

Seismic refraction

Orogeny

10.1093/gji/ggx509

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Main problems of neogeodynamics phenomena investigation and mapping

Technika Poszukiwań Geologicznych (2003)

А. К. Карабанов R. G. Garetsky Р. Е. Айзберг T. Aronova

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Seismotectonic of Belarus and the Baltic sea region

Technika Poszukiwań Geologicznych (1999)

Р. Е. Айзберг R. G. Garetsky A.G. Aronov A. Karabanow О. Сафонов

Baltic sea

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Asymmetry of the deep structure and oil and gas content within the Pripyat Paleorift

Proceedings (1996)

Andrei M. Kovkhuto R. G. Garetsky V. S. Konischev

The Pripyat paleorift is found within the East European Craton and is the western west-east strike segment of the Pripyat- Donets Aulacogene and the part of the Sarmatian-Turanian Lineament - one of the biggest lineaments in the Eurasia.

Lineament

10.3997/2214-4609.201409102

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Peculiarities of Fault Tectonics in Belarus: Investigations and Mapping

Springer eBooks (2006)

Roman Ye Aizberg R. G. Garetsky A. Kovkhuto M.D. Parkhomov

Trough (economics)

Exploration geophysics

Salt tectonics

10.1007/1-4020-3551-9_17

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East European Craton

Elsevier eBooks (2016)

Svetlana Bogdanova Roland Gorbatschev R. G. Garetsky

10.1016/b978-0-08-102908-4.10020-7

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Citations (21)

SIGNIFICANT SCIENTIFIC AND APPLIED RESULTS OF THE INSTITUTE OF NATURE MANAGEMENT OF THE NATIONAL ACADEMY OF SCIENCES OF BELARUS IN THE FIELD OF GEOTECTONICS, GEOPHYSICS AND PETROLEUM GEOLOGY

Nature Management (2022)

Ya. G. Gribik R. G. Garetsky R. E. Girin

A brief analysis of the significant geological results of the last period obtained at the Institute of Nature Management of the National Academy of Sciences of Belarus, presented in the form of two blocks, including projects of fundamental and applied importance, is given. The fundamental developments of this period include studies on the fault tectonics of Belarus, synrift geodynamics of the Pripyat trough, the ecological and tectonophysical environment of Belarus, suture zones on the territory of Belarus, a geological and geophysical model of the deep structure of the Earth's crust according to the Georift-2013 profile, unconventional sources of hydrocarbon raw materials of Belarus. Among the developments of an applied nature are the creation of a model of the oil and geological zoning of the Pripyat trough, the justification of studies on the geological and geophysical profile "Vostochny", the features of the manifestation of natural mercury in the geological environment, the justification of oil work on Poznyakevichskaya Square and systematic studies of priority areas of the Pripyat trough, geological and geophysical studies on the Vechernegorskaya area of Antarctica.

geodynamics

Trough (economics)

Exploration geophysics

10.47612/2079-3928-2022-2-53-67

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Neogeodynamics Phenomena Investigation and Computerized Mapping in Belarus

Springer eBooks (2006)

А. К. Карабанов R. G. Garetsky Р. Е. Айзберг T. Aronova Dmitry Kurlovich

Discontinuity (linguistics)

10.1007/1-4020-3551-9_15

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