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The Bushveld Igneous Complex (BIC) is the largest layered igneous intrusion within the Earth's crust. It has been tilted and eroded forming the outcrops around what appears to be the edge of a great geological basin: the Transvaal Basin. It is approximately two billion years old and is divided into four limbs or lobes: northern, eastern, southern and…
Economy & Art
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complex platinum bushveld within zone chromitite mining chromite rustenburg reef layered fault pyroxenite mineral merensky south layers magma deposits eastern
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Bushveld Igneous Complex | is a | layered mafic intrusion | 0.90 | text |
| chalcopyrite | instance of | and contains Fe-poor sulphides | 0.80 | text |
| pentlandite | instance of | and contains Fe-poor sulphides | 0.80 | text |
| pyrrhotite with minor amounts of galena | instance of | and contains Fe-poor sulphides | 0.80 | text |
| sphalerite.Lower Chromitite | instance of | and contains Fe-poor sulphides | 0.80 | text |
| phlogopite | instance of | interstitial plagioclase and clinopyroxene with minor variable amounts accessory minerals | 0.80 | text |
| mentioned | instance of | and other interstitial phases | 0.80 | text |
| collision | instance of | record of tectonic activity by type of structure | 0.80 | text |
| rifting | instance of | record of tectonic activity by type of structure | 0.80 | text |
| and influence on the evolution of the BIC | instance of | record of tectonic activity by type of structure | 0.80 | text |
| diorite progressively | instance of | 700 m thick and is composed of gabbro and anorthosite which overlays more differentiated rocks | 0.80 | text |
| quartz | instance of | fine to medium-grained norite and gabbronorite with varying amounts of accessory minerals | 0.80 | text |
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