Petrochemical and mineralogical relationships in the Koperberg Suite, Namaqualand, South Africa
The anorthositic to noritic Koperberg suite is distinguished by a dispersed mode of occurrence and primary copper sulphides. Petrographic variation is mainly caused by change in the relative proportions of three rock-forming minerals: andesine orthopyroxene and brown mica. Average major-element chem...
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Veröffentlicht in: | The American mineralogist 1990-02, Vol.75 (1-2), p.27-36 |
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Hauptverfasser: | , |
Format: | Artikel |
Sprache: | eng |
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Zusammenfassung: | The anorthositic to noritic Koperberg suite is distinguished by a dispersed mode of occurrence and primary copper sulphides. Petrographic variation is mainly caused by change in the relative proportions of three rock-forming minerals: andesine orthopyroxene and brown mica. Average major-element chemical compositions are calculated for the principal rock types. |
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ISSN: | 0003-004X 1945-3027 |