Conditions of formation of ferruginous rocks of the Middle Bug area

An opinion has been substantiated that the rocks of ferruginous-siliceous-carbonate formation of the Bug and Golovanev suture zone are endogenous. Their appearance is synchronous with the appearance of rocks of the Gadantsev suite of the Krivoy Rog–Kremenchug zone.  Peculiarities of this formation a...

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Datum:2015
1. Verfasser: Usenko, O.
Format: Artikel
Sprache:Russisch
Veröffentlicht: S. Subbotin Institute of Geophysics of the NAS of Ukraine 2015
Online Zugang:https://journals.uran.ua/geofizicheskiy/article/view/111122
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Geofizicheskiy Zhurnal
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author Usenko, O.
author_facet Usenko, O.
author_sort Usenko, O.
baseUrl_str
collection OJS
datestamp_date 2020-10-07T11:38:58Z
description An opinion has been substantiated that the rocks of ferruginous-siliceous-carbonate formation of the Bug and Golovanev suture zone are endogenous. Their appearance is synchronous with the appearance of rocks of the Gadantsev suite of the Krivoy Rog–Kremenchug zone.  Peculiarities of this formation and of enclosing strata of the Bug series can be explained by behavior of the geodynamic  process, sharp change of composition of deep fluid which accompanied differentiation of asthenospheric melt as well as crystallization under conditions of granulite metamorphism facies. Specific composition of rocks of this formation depends on mixing of the residual water chloride-potassium and deep carbonate-fluoride-sodium fluids.
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spelling journalsuranua-geofizicheskiy-article-1111222020-10-07T11:38:58Z Conditions of formation of ferruginous rocks of the Middle Bug area Usenko, O. An opinion has been substantiated that the rocks of ferruginous-siliceous-carbonate formation of the Bug and Golovanev suture zone are endogenous. Their appearance is synchronous with the appearance of rocks of the Gadantsev suite of the Krivoy Rog–Kremenchug zone.  Peculiarities of this formation and of enclosing strata of the Bug series can be explained by behavior of the geodynamic  process, sharp change of composition of deep fluid which accompanied differentiation of asthenospheric melt as well as crystallization under conditions of granulite metamorphism facies. Specific composition of rocks of this formation depends on mixing of the residual water chloride-potassium and deep carbonate-fluoride-sodium fluids. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2015-08-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/111122 10.24028/gzh.0203-3100.v37i4.2015.111122 Geofizicheskiy Zhurnal; Vol. 37 No. 4 (2015); 32-50 Геофизический журнал; Том 37 № 4 (2015); 32-50 Геофізичний журнал; Том 37 № 4 (2015); 32-50 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/111122/105991 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
spellingShingle Usenko, O.
Conditions of formation of ferruginous rocks of the Middle Bug area
title Conditions of formation of ferruginous rocks of the Middle Bug area
title_full Conditions of formation of ferruginous rocks of the Middle Bug area
title_fullStr Conditions of formation of ferruginous rocks of the Middle Bug area
title_full_unstemmed Conditions of formation of ferruginous rocks of the Middle Bug area
title_short Conditions of formation of ferruginous rocks of the Middle Bug area
title_sort conditions of formation of ferruginous rocks of the middle bug area
url https://journals.uran.ua/geofizicheskiy/article/view/111122
work_keys_str_mv AT usenkoo conditionsofformationofferruginousrocksofthemiddlebugarea