Regularities in the formation of manganese deposits on continents
The destructive type of tectonic regimes directly controlled the formation of the larger part of primary manganese deposits. Recurrences of these regimes in the history of the Earth marked the periodicity of the active manganese-forming epochs. The main body of the manganese ores was deposited in as...
Elmentve itt :
| Szerző: | |
|---|---|
| Dokumentumtípus: | Cikk |
| Megjelent: |
University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Szeged
1986
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| Sorozat: | Acta mineralogica-petrographica
28 |
| Kulcsszavak: | Kőzettan, Ásványtan, Földtan |
| Tárgyszavak: | |
| Online Access: | http://acta.bibl.u-szeged.hu/24745 |