Informace o publikaci
The genesis of the precambrian so-called iron formations (Sydvaranger type) within the gneiss of the Desná Dome, Hrubý Jeseník Mts., Czech Republic
| Autoři | |
|---|---|
| Rok publikování | 2002 |
| Druh | Článek ve sborníku |
| Konference | Mineralogical Society of Poland - Special Papers |
| Fakulta / Pracoviště MU | |
| Citace | |
| Obor | Geologie a mineralogie |
| Klíčová slova | iron formation; magnetite; Desná Dome; Silesicum |
| Popis | By definition iron formations are of sedimentary origin. However, the magnetite ores of the Desná Dome in Silesicum were formed under magmatic conditions and are metamorphosed and silicified equivalents of iron-rich basic rocks and thus similar to the Itakpe type deposit of Nigeria (Mücke, Neumann 1986) which was previously described as iron formation (Olade 1982). |
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