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

Authors

  • O. Usenko S.I. Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine, Kyiv, Ukraine

DOI:

https://doi.org/10.24028/gzh.0203-3100.v37i1.2015.111321

Keywords:

ferruginous formations, the Archean, greenstone structures, physical-chemical interactions, paleo-geodynamic process, hydrothermal ore deposition, the thickness of lithosphere

Abstract

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.

References

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Published

2015-02-01

How to Cite

Usenko, O. (2015). Conditions of ferruginous-cherty formations origin (Middle-Dnieper mega-block). Geofizicheskiy Zhurnal, 37(1), 21–41. https://doi.org/10.24028/gzh.0203-3100.v37i1.2015.111321

Issue

Vol. 37 No. 1 (2015)

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Articles

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