| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 5785674 | Journal of African Earth Sciences | 2017 | 14 Pages |
â¢Basaltic rocks formed in an oceanic plateau setting above plume-head.â¢Gold endowment interpreted to be linked with plume-related basaltic rocks.â¢Two geochemical diagrams using Zr, Y, Nb and Th for establishing the gold fertility of belts.
Birimian volcanic rocks of the Mana District are located in the an important gold-mineralized segment of the Paleoproterozoic Houndé greenstone belt, western Burkina Faso, which contains cumulative resources of â¼11 Moz. Five orogenic gold deposits (â¼8 Moz) are hosted in or close to basaltic rocks. Theses rocks were studied to investigate their possible role as a gold source in younger orogenic gold deposits. They are Fe-rich tholeiitic basalts with flat REE patterns, with (La/Yb)N = 0.96-1.3 and without negative Eu anomaly (Eu/Eu* = 0.92-1.26). The basalts also have low initial Sr isotopic ratios (0.693612-0.702190) and positive εNd values (+2.25 to +3.14). Using a Ce/Nb vs. Th/Nb diagram and various plume-related basalts worldwide for comparison, the Mana basalts are shown to be plume-related. In addition, using Zr/Nb vs. Nb/Th and Nb/Y vs. Zr/Y binary diagrams and reference fields, the Mana basaltic rocks appear to have formed directly above the plume head. Because plume-related basalts tend to be enriched in gold relative to MORB, we propose that the gold endowment of the Mana district is mostly related to the occurrence of plume-related basaltic rocks, which may have served as an important metal stock during subsequent remobilization for forming the orogenic gold deposits. We also propose that for gold exploration, two simple geochemical diagrams involving Zr, Y, Nb and Th could be used at an early stage to test the origin of the basaltic rocks and hence indirectly establish the fertility of a specific belt for hosting orogenic gold deposits.
Graphical abstractDownload high-res image (445KB)Download full-size image
