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...
Bewaard in:
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| Formaat: | Artigo |
| Taal: | Inglês |
| Gepubliceerd in: |
Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine
2015-02-01
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| Reeks: | Геофизический журнал |
| Onderwerpen: | |
| Online toegang: | https://journals.uran.ua/geofizicheskiy/article/view/111321 |
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