Geology Reference
In-Depth Information
Zirconium
Zinc
Wolfram
Vanadium
Uranium
Titanium-ilmenite
Titanium-rutile
Tin
Thorium
Tellurium
Tantalum
Strontium
Silver
Silicon
Selenium
Rhenium
REE
Potash
PGM
Phosphate rock
Niobium
Nickel - laterites
Nickel - sulfides
Molybdenum
Mercury
Manganese
Magnesium
Lithium
Limestone
Lead
Iron ore
Iodine
Indium
Helium
Gypsum
Graphite
Gold
Germanium
Gallium
Fluorspar
Feldspar
Copper
Cobalt
Chromium
Cesium
Cadmium
Boron
Bismuth
Beryllium
Barium
Arsenic
Antimony
Aluminium (Bauxite)
3,500,000,000
Production, tons
3,000,000,000
2,500,000,000
2,000,000,000
1,500,000,000
Phosphate rock
Limestone
1,000,000,000
Iron ore
500,000,000
Gypsum
Aluminium
0
Fig. 13.31
Production of the main non-fuel mineral commodities on Earth in the 20th century
Zirconium
Zinc
Wolfram
Vanadium
Uranium
Titanium-ilmenite
Titanium-rutile
Tin
Thorium
Tellurium
Tantalum
Strontium
Silver
Silicon
Selenium
Rhenium
REE
Potash
PGM
Niobium
Nickel - laterites
Nickel - sulfides
Molybdenum
Mercury
Manganese
Magnesium
Lithium
Lead
Iodine
Indium
Helium
Graphite
Gold
Germanium
Gallium
Fluorspar
Feldspar
Copper
Cobalt
Chromium
Cesium
Cadmium
Boron
Bismuth
Beryllium
Barium
Arsenic
Antimony
180,000,000
Production, tons
160,000,000
140,000,000
120,000,000
Zinc
100,000,000
Titanium
Silver
80,000,000
Potash
Manganese
60,000,000
Magnesium
Lead
Fluorspar
40,000,000
Feldspar
Copper
20,000,000
Chromium
Boron
Barium
0
Fig. 13.32 Production of the main non-fuel mineral commodities on Earth in the 20th century,
excluding aluminium, iron, gypsum, phosphate rock and limestone
The total natural bonus lost associated with the dispersion of the non-fuel mi-
nerals analysed is near 100 Gtoe. This means that to replace all dispersed non-fuel
mineral commodities with current technology, one would require about a third of
all available fuel oil reserves on Earth (346 Gtoe Table 11.20).
Excluding potash, iron and aluminium, which eclipse the rest of the commodi-
ties, one can observe in Fig. 13.34 that in decreasing order, the production of gold,
 
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