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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| Datum: | 2015 |
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| Format: | Artikel |
| Sprache: | Russisch |
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S. Subbotin Institute of Geophysics of the NAS of Ukraine
2015
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| Online Zugang: | https://journals.uran.ua/geofizicheskiy/article/view/111321 |
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| Назва журналу: | Geofizicheskiy Zhurnal |
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Geofizicheskiy Zhurnal| _version_ | 1856543166219419649 |
|---|---|
| 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. |
| first_indexed | 2025-07-17T11:05:45Z |
| format | Article |
| id | journalsuranua-geofizicheskiy-article-111321 |
| institution | Geofizicheskiy Zhurnal |
| language | Russian |
| last_indexed | 2025-07-17T11:05:45Z |
| publishDate | 2015 |
| publisher | S. Subbotin Institute of Geophysics of the NAS of Ukraine |
| record_format | ojs |
| 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 |
| work_keys_str_mv | AT usenkoo conditionsofferruginouschertyformationsoriginmiddledniepermegablock |