On plotting the scheme of fracture-mega-block tectonics of the Ukrainian Shield in a scale 1 : 500 000

The main principles have been proposed for discussion on composing the Scheme of fracrture-mega-block tectonics of the Ukrainian Shield in a scale 1 : 500 000 supported by a decision of Inter-departmental tectonic committee of Ukraine as a basis for plotting the Tectonic map of the Ukrainian Shield...

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Datum:2017
Hauptverfasser: Gintov, O.B., Yentin, V.A., Mychak, S.V.
Format: Artikel
Sprache:Ukrainian
Veröffentlicht: Subbotin Institute of Geophysics of the NAS of Ukraine 2017
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Online Zugang:https://journals.uran.ua/geofizicheskiy/article/view/112340
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spelling journalsuranua-geofizicheskiy-article-1123402020-02-13T14:21:03Z On plotting the scheme of fracture-mega-block tectonics of the Ukrainian Shield in a scale 1 : 500 000 Gintov, O.B. Yentin, V.A. Mychak, S.V. the Ukrainian Shield mega-block fracture zone structural-formational complex geophysical fields shearing zones The main principles have been proposed for discussion on composing the Scheme of fracrture-mega-block tectonics of the Ukrainian Shield in a scale 1 : 500 000 supported by a decision of Inter-departmental tectonic committee of Ukraine as a basis for plotting the Tectonic map of the Ukrainian Shield in the mentioned scale. The existing maps and schemes of the blocky subdivision of the Ukrainian Shield considerably differ from each other especially because the fact that the unified principles of blocky and especially mega-blocky subdivision for the whole shield were not yet formulated then and the criteria for subdivision and mapping of inter-mega-block fracture zones were not supported. Such criteria are being considered in this work, and examples of schemes of fracture-block tectonics of three sheets in a scale 1 : 200 000 composed on their base have been given. It is proved that the Scheme of fracture-mega-block structure of the Ukrainian Shield must reflect the present-day blocky subdivision of the earth crust formed at the border of Early and Middle Proterozoic, at the very end of establishment of the granite socle of the shield. Only such mega-blocks and blocks and in the first place fault zones, which separate them, may be exactly identified and mapped that is an important condition, because the most part of deposits and ore manifestations of the shield are just related to the fracture zones. More ancient margins of mega-blocks and fault zones in the areas of Early Proterozoic tectonic-magmatic activation are hypothetical and cannot be mapped unambiguously. It has been shown that while plotting the Scheme of fracture-mega-block tectonics of the Ukrainian Shield the priority belongs to geophysical methods. Subbotin Institute of Geophysics of the NAS of Ukraine 2017-10-26 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/112340 10.24028/gzh.0203-3100.v39i5.2017.112340 Geofizicheskiy Zhurnal; Vol. 39 No. 5 (2017); 63-82 Геофизический журнал; Том 39 № 5 (2017); 63-82 Геофізичний журнал; Том 39 № 5 (2017); 63-82 2524-1052 0203-3100 uk https://journals.uran.ua/geofizicheskiy/article/view/112340/195742 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
institution Geofizicheskiy Zhurnal
baseUrl_str
datestamp_date 2020-02-13T14:21:03Z
collection OJS
language Ukrainian
topic the Ukrainian Shield
mega-block
fracture zone
structural-formational complex
geophysical fields
shearing zones
spellingShingle the Ukrainian Shield
mega-block
fracture zone
structural-formational complex
geophysical fields
shearing zones
Gintov, O.B.
Yentin, V.A.
Mychak, S.V.
On plotting the scheme of fracture-mega-block tectonics of the Ukrainian Shield in a scale 1 : 500 000
topic_facet the Ukrainian Shield
mega-block
fracture zone
structural-formational complex
geophysical fields
shearing zones
format Article
author Gintov, O.B.
Yentin, V.A.
Mychak, S.V.
author_facet Gintov, O.B.
Yentin, V.A.
Mychak, S.V.
author_sort Gintov, O.B.
title On plotting the scheme of fracture-mega-block tectonics of the Ukrainian Shield in a scale 1 : 500 000
title_short On plotting the scheme of fracture-mega-block tectonics of the Ukrainian Shield in a scale 1 : 500 000
title_full On plotting the scheme of fracture-mega-block tectonics of the Ukrainian Shield in a scale 1 : 500 000
title_fullStr On plotting the scheme of fracture-mega-block tectonics of the Ukrainian Shield in a scale 1 : 500 000
title_full_unstemmed On plotting the scheme of fracture-mega-block tectonics of the Ukrainian Shield in a scale 1 : 500 000
title_sort on plotting the scheme of fracture-mega-block tectonics of the ukrainian shield in a scale 1 : 500 000
description The main principles have been proposed for discussion on composing the Scheme of fracrture-mega-block tectonics of the Ukrainian Shield in a scale 1 : 500 000 supported by a decision of Inter-departmental tectonic committee of Ukraine as a basis for plotting the Tectonic map of the Ukrainian Shield in the mentioned scale. The existing maps and schemes of the blocky subdivision of the Ukrainian Shield considerably differ from each other especially because the fact that the unified principles of blocky and especially mega-blocky subdivision for the whole shield were not yet formulated then and the criteria for subdivision and mapping of inter-mega-block fracture zones were not supported. Such criteria are being considered in this work, and examples of schemes of fracture-block tectonics of three sheets in a scale 1 : 200 000 composed on their base have been given. It is proved that the Scheme of fracture-mega-block structure of the Ukrainian Shield must reflect the present-day blocky subdivision of the earth crust formed at the border of Early and Middle Proterozoic, at the very end of establishment of the granite socle of the shield. Only such mega-blocks and blocks and in the first place fault zones, which separate them, may be exactly identified and mapped that is an important condition, because the most part of deposits and ore manifestations of the shield are just related to the fracture zones. More ancient margins of mega-blocks and fault zones in the areas of Early Proterozoic tectonic-magmatic activation are hypothetical and cannot be mapped unambiguously. It has been shown that while plotting the Scheme of fracture-mega-block tectonics of the Ukrainian Shield the priority belongs to geophysical methods.
publisher Subbotin Institute of Geophysics of the NAS of Ukraine
publishDate 2017
url https://journals.uran.ua/geofizicheskiy/article/view/112340
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