The Cu-Zn Obrazek ore deposit, Czechoslovakia: A volcanogenic deposit included in the Ransko intrusive complex
Autor: | David H. Watkinson, P. R. Mainwaring, Zdeněk Pertold |
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Rok vydání: | 1978 |
Předmět: | |
Zdroj: | Mineralium Deposita. 13 |
ISSN: | 1432-1866 0026-4598 |
DOI: | 10.1007/bf00204639 |
Popis: | The Cu-Zn Obrazek ore deposit is reinterpreted as metamorphosed volcanogenic-type rather than epigenetic vein-type. Enclosed by undeformed, non-metamorphosed mafic-ultramafic rocks of the Ransko complex, the ore is a highly folded, intensely metamorphosed (Zn-rich) association of banded, massive sphalerite-barite-pyrite-pyrrhotite-chalcopyrite and (Cu-rich)pyrite-chalcopyrite-pyrrhotite. Cu-rich ores are disseminated in deformed metamorphic assemblages of quartz, sillimanite, cordierite, anthophyllite, orthopyroxene and gahnite. Textural and compositional features in the metamorphic rocks suggest that the cordierite-anthophyllite assemblage was produced by regional metamorphism of rocks associated with the ore deposit. Inclusion of the Cu-Zn deposit and associated rocks in the Ransko intrusive complex produced contact metamorphic hornfelses of quartz, cordierite, orthopyroxene and Al-spinel. The occurrence and compositions of Zn-rich chromian spinel and minor intercumulus sulfides in anorthosite, troctolite and norite of the Ransko complex near the Obrazek ore body are interpreted to result from contamination of the Ransko parent magma by the Cu-Zn deposit and associated rocks. |
Databáze: | OpenAIRE |
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