Anoxic environment and formation of superlarge ore deposits
The formation of many metallic and non-metallic ore deposits is a result of coupling of mineralization, related to anoxic environment and regional, or global background. Inter act~on, concordance and continual development of the mineralization and environmental background control the large to superl...
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Veröffentlicht in: | Science China. Earth sciences 1998-04, Vol.41 (S1), p.37-46 |
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Hauptverfasser: | , , |
Format: | Artikel |
Sprache: | eng |
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Online-Zugang: | Volltext |
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Zusammenfassung: | The formation of many metallic and non-metallic ore deposits is a result of coupling of mineralization, related to anoxic environment and regional, or global background. Inter act~on, concordance and continual development of the mineralization and environmental background control the large to superlarge scale of ore deposits. Three kinds of ore-forming models related to anoxic environment and three important background patterns are suggested. The turning period of geological history is favorable to the formation of large to superlarge ore deposits.[PUBLICATION ABSTRACT] |
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ISSN: | 1006-9313 1674-7313 1862-2801 1869-1897 |
DOI: | 10.1007/BF02875636 |