Base metal-tin association(f)

Ilmenite and magnetite in basalts and dolerites(a,b)

Polishing characteristics and problems(a,f)

Adventitiously introduced metals and grinding grit, dried immersion oil and amalgam(a)

Ilmenite and magnetite in basalts and dolerites(a-f)

Altered iron-titanium oxides in alkali olivine basalt(a,b,e)

Chromite associations(f)

Sulphides within ultramafic rocks in ophiolites(a)

Magmatic nickel ores(f)

Magmatic sulphide ores(f)

Magmatic sulphides(d,f)

Carbonatites(b-d)

Unmineralized intermediate rocks(a,b,d)

Slightly mineralized granites(f)

Porphyry copper ores(c)

Porphyry copper and molybdenum ores(f)

Massive sulphides in ophiolites(c)

Oxide placer deposits(a)

Manganese minerals(c-f)

Iron formations and bauxite(a-c)

Metamorphosed sulphides(f)

Appalachian metamorphosed sulphides(b,f)

Skarns( b-f)

Supergene alteration (f)

Clastic-hosted copper ores(c)

Skarns(c)

Unmineralized sandstones(a,b,e)

Oxide placer deposits(a)

Iron formations and bauxite(d)

Silver-nickel-cobalt-arsenic-bismuth±uranium. The five metals association.(c-e)

Sulphides within ultramafic rocks in ophiolites(b,d-f)

Nickel-rich assemblages within Mississippi Valley-style mineralization(c,d)

Slightly mineralized granites(d,f)

Minor sulphide mineralization in granite(d,e)

Porphyry copper ores(e)

Porphyry copper and molybdenum ores(d-f)

Porphyry-style tin-tungsten-molybdenum ores(c-e)

Mississippi Valley-style lead-zinc deposits(f)