Polishing characteristics and problems(b,f)
Adventitiously introduced metals and grinding grit, dried immersion oil and amalgam(a)
Ilmenite and magnetite in basalts and dolerites(c,f)
Altered iron-titanium oxides in alkali olivine basalt(a,c-f)
Magmatic iron-titanium ores (b,c)
Unmineralized intermediate rocks(a,b,e)
Porphyry copper and molybdenum ores(a-c)
Massive sulphides in ophiolites(f)
Massive sulphides within ophiolites(a)
High-temperature tin-tungsten-bismuth mineralization(e)
Copper, iron and low temperature tin mineralization(d)
Clay ironstones and oolitic iron ores(c-f)
Iron formations and bauxite(a-f)
Supergene enrichment of copper ores( a-f)
HaemoilmeniteMagmatic iron-titanium ores(a-f)
Unmineralized intermediate rocks(e,f)
HeazlewooditeSulphides within ultramafic rocks in ophiolites(a-f)
HessiteTellurides associated with gold mineralization(e)