Bohmke reef: platinum-group element mineralization associated with C1d chromitite of the Great Dyke, Zimbabwe
- Organization:
- The Institute of Materials, Minerals and Mining
- Pages:
- 7
- File Size:
- 3679 KB
- Publication Date:
- Apr 1, 1996
Abstract
The reef is a PGE-enriched sulphidic zone, stratigraphically associated with and overlapping the C1d chromitite layer, that was formed by magmatic processes at the 1e-1d subunit boundary. Two distinct patterns of PGE enrichment are related to the presence or absence of Cr2O3 oversaturation during sulphide liquation that occurred during a complex sequence of changes at this boundary
Citation
APA: (1996) Bohmke reef: platinum-group element mineralization associated with C1d chromitite of the Great Dyke, Zimbabwe
MLA: Bohmke reef: platinum-group element mineralization associated with C1d chromitite of the Great Dyke, Zimbabwe. The Institute of Materials, Minerals and Mining, 1996.