Neogeodynamics at northern prospect area of Petrikov potash deposit

The results of studies of neogeodynamics at northern prospect area of Petrikov potash deposit in Belarus are discussed. Endogenic and exogenic processes, active since the Late Oligocene have been studied with the complex of methods, including lineament and structural-geomorphological analysis. As a...

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Main Authors: Dzmitry V. Barbikov, Dzmitry M. Kurlovich, Vitali E. Kutyrlo
Format: Article
Language:Belarusian
Published: Belarusian State University 2017-10-01
Series: Журнал Белорусского государственного университета: География, геология
Subjects:
Online Access:https://journals.bsu.by/index.php/geography/article/view/993
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spelling doaj-eaed538fa7834ffdb0fd7b29b3942e772020-11-25T02:37:48ZbelBelarusian State University Журнал Белорусского государственного университета: География, геология2521-67402617-39722017-10-012175183993Neogeodynamics at northern prospect area of Petrikov potash depositDzmitry V. Barbikov0Dzmitry M. Kurlovich1Vitali E. Kutyrlo2JSC «Belaruskali», Korzh Street, 5, 223710, Soligorsk, BelarusBelarusian State University, Niezaliežnasci Avenue, 4, 220030, Minsk, BelarusJSC «Belgorkhimprom», Masherov Avenue, 17, 220029, Minsk, BelarusThe results of studies of neogeodynamics at northern prospect area of Petrikov potash deposit in Belarus are discussed. Endogenic and exogenic processes, active since the Late Oligocene have been studied with the complex of methods, including lineament and structural-geomorphological analysis. As a result of lineament analysis, it was determined that the most area of Northern prospect of Petrikov potash deposit is stable in terms of geodynamics. The zones of potential development of neogeodynamic processes occupy only 20 % of the area of prospect. These zones are referred to areas of weakened earth crust, within which higher fracturing of rocks may occur. Based on the results of structural-geomorphological analysis, geodynamic active structures and lineament are revealed. Geodynamic activity of the territory since the end of Middle Pleistocene is defined. During the period from the end of Middle Pleistocene to Holocene, a weak intensity of geodynamic processes occurred for 54 % of total area of Northern prospect, a moderate intensity was registered for 33 %, and higher than moderate and high intensity was characteristic for 13 % of total area. In Holocene a weak intensity of recent geodynamic processes is registered for 78 % of the research area, moderate intensity is relevant to 9 %, and higher than moderate intensity is recorded for 3 % of study area. The received results are considered at design and construction of especially important engineering constructions of Petrikovsky ore-dressing and processing enterprise.https://journals.bsu.by/index.php/geography/article/view/993geodynamicslineamentlineaments densitymorphostructuresneogeodynamic active structureszones of neogeodynamic activitygeographic information systems
collection DOAJ
language Belarusian
format Article
sources DOAJ
author Dzmitry V. Barbikov
Dzmitry M. Kurlovich
Vitali E. Kutyrlo
spellingShingle Dzmitry V. Barbikov
Dzmitry M. Kurlovich
Vitali E. Kutyrlo
Neogeodynamics at northern prospect area of Petrikov potash deposit
Журнал Белорусского государственного университета: География, геология
geodynamics
lineament
lineaments density
morphostructures
neogeodynamic active structures
zones of neogeodynamic activity
geographic information systems
author_facet Dzmitry V. Barbikov
Dzmitry M. Kurlovich
Vitali E. Kutyrlo
author_sort Dzmitry V. Barbikov
title Neogeodynamics at northern prospect area of Petrikov potash deposit
title_short Neogeodynamics at northern prospect area of Petrikov potash deposit
title_full Neogeodynamics at northern prospect area of Petrikov potash deposit
title_fullStr Neogeodynamics at northern prospect area of Petrikov potash deposit
title_full_unstemmed Neogeodynamics at northern prospect area of Petrikov potash deposit
title_sort neogeodynamics at northern prospect area of petrikov potash deposit
publisher Belarusian State University
series Журнал Белорусского государственного университета: География, геология
issn 2521-6740
2617-3972
publishDate 2017-10-01
description The results of studies of neogeodynamics at northern prospect area of Petrikov potash deposit in Belarus are discussed. Endogenic and exogenic processes, active since the Late Oligocene have been studied with the complex of methods, including lineament and structural-geomorphological analysis. As a result of lineament analysis, it was determined that the most area of Northern prospect of Petrikov potash deposit is stable in terms of geodynamics. The zones of potential development of neogeodynamic processes occupy only 20 % of the area of prospect. These zones are referred to areas of weakened earth crust, within which higher fracturing of rocks may occur. Based on the results of structural-geomorphological analysis, geodynamic active structures and lineament are revealed. Geodynamic activity of the territory since the end of Middle Pleistocene is defined. During the period from the end of Middle Pleistocene to Holocene, a weak intensity of geodynamic processes occurred for 54 % of total area of Northern prospect, a moderate intensity was registered for 33 %, and higher than moderate and high intensity was characteristic for 13 % of total area. In Holocene a weak intensity of recent geodynamic processes is registered for 78 % of the research area, moderate intensity is relevant to 9 %, and higher than moderate intensity is recorded for 3 % of study area. The received results are considered at design and construction of especially important engineering constructions of Petrikovsky ore-dressing and processing enterprise.
topic geodynamics
lineament
lineaments density
morphostructures
neogeodynamic active structures
zones of neogeodynamic activity
geographic information systems
url https://journals.bsu.by/index.php/geography/article/view/993
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