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 |
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Subbotin Institute of Geophysics of the NAS of Ukraine
2012
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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 |
work_keys_str_mv |
AT mychaksv deflectedmodeandkinematiccharacteristicsoftheupperpartoftheearthscrustintheareaofthemichurinskdepositkirovogradoreareaoftheukrainianshield |
first_indexed |
2024-04-21T19:41:02Z |
last_indexed |
2024-04-21T19:41:02Z |
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1796974536197931008 |