Deflected mode and kinematic characteristics of the upper part of the earth’s crust in the area of the Michurinsk deposit (Kirovograd ore area) of the Ukrainian Shield

The results of the tectonophysical research carried out in 2010 in the central part of the Ukrainian shield near the Michurinsk uranium deposit are given in this article. The internal structure and stress-strained state of the Earth’s crust have been investigated by the results of the structural and...

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Дата:2012
Автор: Mychak, S.V.
Формат: Стаття
Мова:rus
Опубліковано: Subbotin Institute of Geophysics of the NAS of Ukraine 2012
Онлайн доступ:https://journals.uran.ua/geofizicheskiy/article/view/116624
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Назва журналу:Geofizicheskiy Zhurnal

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Geofizicheskiy Zhurnal
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spelling journalsuranua-geofizicheskiy-article-1166242020-10-07T12:21:24Z Deflected mode and kinematic characteristics of the upper part of the earth’s crust in the area of the Michurinsk deposit (Kirovograd ore area) of the Ukrainian Shield Mychak, S.V. The results of the tectonophysical research carried out in 2010 in the central part of the Ukrainian shield near the Michurinsk uranium deposit are given in this article. The internal structure and stress-strained state of the Earth’s crust have been investigated by the results of the structural and paragenetic fracturing analysis as well as the stress fields by the data of measurements of the fault slip. It was established that the ore-forming phase of deformation within the deposit was the Bobrinetsk-Zhivanovsk shear-thrust one during which a crack separation and extension structures were formed. The redistribution of the ore substance occurred in the Subbotsk-Moshorinsk and Korsun-Novomirgorod stages. Subbotin Institute of Geophysics of the NAS of Ukraine 2012-04-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116624 10.24028/gzh.0203-3100.v34i2.2012.116624 Geofizicheskiy Zhurnal; Vol. 34 No. 2 (2012); 125-133 Геофизический журнал; Том 34 № 2 (2012); 125-133 Геофізичний журнал; Том 34 № 2 (2012); 125-133 2524-1052 0203-3100 rus https://journals.uran.ua/geofizicheskiy/article/view/116624/110658 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
institution Geofizicheskiy Zhurnal
collection OJS
language rus
format Article
author Mychak, S.V.
spellingShingle Mychak, S.V.
Deflected mode and kinematic characteristics of the upper part of the earth’s crust in the area of the Michurinsk deposit (Kirovograd ore area) of the Ukrainian Shield
author_facet Mychak, S.V.
author_sort Mychak, S.V.
title Deflected mode and kinematic characteristics of the upper part of the earth’s crust in the area of the Michurinsk deposit (Kirovograd ore area) of the Ukrainian Shield
title_short Deflected mode and kinematic characteristics of the upper part of the earth’s crust in the area of the Michurinsk deposit (Kirovograd ore area) of the Ukrainian Shield
title_full Deflected mode and kinematic characteristics of the upper part of the earth’s crust in the area of the Michurinsk deposit (Kirovograd ore area) of the Ukrainian Shield
title_fullStr Deflected mode and kinematic characteristics of the upper part of the earth’s crust in the area of the Michurinsk deposit (Kirovograd ore area) of the Ukrainian Shield
title_full_unstemmed Deflected mode and kinematic characteristics of the upper part of the earth’s crust in the area of the Michurinsk deposit (Kirovograd ore area) of the Ukrainian Shield
title_sort deflected mode and kinematic characteristics of the upper part of the earth’s crust in the area of the michurinsk deposit (kirovograd ore area) of the ukrainian shield
description The results of the tectonophysical research carried out in 2010 in the central part of the Ukrainian shield near the Michurinsk uranium deposit are given in this article. The internal structure and stress-strained state of the Earth’s crust have been investigated by the results of the structural and paragenetic fracturing analysis as well as the stress fields by the data of measurements of the fault slip. It was established that the ore-forming phase of deformation within the deposit was the Bobrinetsk-Zhivanovsk shear-thrust one during which a crack separation and extension structures were formed. The redistribution of the ore substance occurred in the Subbotsk-Moshorinsk and Korsun-Novomirgorod stages.
publisher Subbotin Institute of Geophysics of the NAS of Ukraine
publishDate 2012
url https://journals.uran.ua/geofizicheskiy/article/view/116624
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first_indexed 2024-04-21T19:41:02Z
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