Conditions of ferruginous-cherty formations origin (Middle-Dnieper mega-block)

The basic idea of existing hypotheses of ferruginous-cherty formations origin is an opinion that the form of iron presence depends on conditions at the depth of sediments accumulation. It has been shown in this paper with Middle-Dnieper mega-block of the Ukrainian Shield greenstone structures used a...

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Date:2015
Main Author: Usenko, O.
Format: Article
Language:Russian
Published: S. Subbotin Institute of Geophysics of the NAS of Ukraine 2015
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Online Access:https://journals.uran.ua/geofizicheskiy/article/view/111321
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Journal Title:Geofizicheskiy Zhurnal

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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 2020-10-07T11:41:07Z
description The basic idea of existing hypotheses of ferruginous-cherty formations origin is an opinion that the form of iron presence depends on conditions at the depth of sediments accumulation. It has been shown in this paper with Middle-Dnieper mega-block of the Ukrainian Shield greenstone structures used as an example that composition of volcanogenic and ferruginous rocks is specified by succession of physical-chemical interactions on the roof of the layer with partial melting.
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publisher S. Subbotin Institute of Geophysics of the NAS of Ukraine
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spelling journalsuranua-geofizicheskiy-article-1113212020-10-07T11:41:07Z Conditions of ferruginous-cherty formations origin (Middle-Dnieper mega-block) Usenko, O. ferruginous formations the Archean greenstone structures physical-chemical interactions paleo-geodynamic process hydrothermal ore deposition the thickness of lithosphere The basic idea of existing hypotheses of ferruginous-cherty formations origin is an opinion that the form of iron presence depends on conditions at the depth of sediments accumulation. It has been shown in this paper with Middle-Dnieper mega-block of the Ukrainian Shield greenstone structures used as an example that composition of volcanogenic and ferruginous rocks is specified by succession of physical-chemical interactions on the roof of the layer with partial melting. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2015-02-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/111321 10.24028/gzh.0203-3100.v37i1.2015.111321 Geofizicheskiy Zhurnal; Vol. 37 No. 1 (2015); 21-41 Геофизический журнал; Том 37 № 1 (2015); 21-41 Геофізичний журнал; Том 37 № 1 (2015); 21-41 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/111321/106319 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
spellingShingle ferruginous formations
the Archean
greenstone structures
physical-chemical interactions
paleo-geodynamic process
hydrothermal ore deposition
the thickness of lithosphere
Usenko, O.
Conditions of ferruginous-cherty formations origin (Middle-Dnieper mega-block)
title Conditions of ferruginous-cherty formations origin (Middle-Dnieper mega-block)
title_full Conditions of ferruginous-cherty formations origin (Middle-Dnieper mega-block)
title_fullStr Conditions of ferruginous-cherty formations origin (Middle-Dnieper mega-block)
title_full_unstemmed Conditions of ferruginous-cherty formations origin (Middle-Dnieper mega-block)
title_short Conditions of ferruginous-cherty formations origin (Middle-Dnieper mega-block)
title_sort conditions of ferruginous-cherty formations origin (middle-dnieper mega-block)
topic ferruginous formations
the Archean
greenstone structures
physical-chemical interactions
paleo-geodynamic process
hydrothermal ore deposition
the thickness of lithosphere
topic_facet ferruginous formations
the Archean
greenstone structures
physical-chemical interactions
paleo-geodynamic process
hydrothermal ore deposition
the thickness of lithosphere
url https://journals.uran.ua/geofizicheskiy/article/view/111321
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