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Appendix E
TYPES OF TITANIUM ORE DEPOSI IS
Ilmenite and Leucoxene
The primary occurrence of ilmenite (Table 44) is in association with
magnetite (Fe3O4) and hematite (Fe2O3) in hard rock deposits.
Such t itaniferous ores are highly variable in ilmenite and iron oxide
content; in the size and physical interlocking of ilmenite and iron oxide
mineral part icles; and in associated oxides, sulf ides, and silicates that
include vanadium, chromium, nickel, aluminum, calcium, magnesium,
zirconium, and other elements. Ilmenite and associated leucoxene also
occur in beach and alluvial sands that are the erosional remnants of
formerly massive or disseminated hard rock deposits. Conditions that
favor natural upgrading of ilmenite to leucoxene in placer deposits are a
tropical climate and location above the water table.
Rut lie and Anatase
Commercial occurrences of rutile (and of its not yet commercialized,
slightly softer and lighter sister oxide, anatase) are mostly in beach
sand deposits in which they are associated with ilmenite and leucoxene
and with several other hard and heavy minerals. Rutile and anatase also
are common components of complex igneous rocks but rarely at a high
enough grade for commercial recovery (Tables 45 and 46~. Rutile is a
component of the U. S. National Stockpile. Its chemical and physical
specifications appear in Appendix G.
Perovskite and Sphene
Although occurrence of perovskite and sphene in complex igneous rocks
is not uncommon, neither mineral is produced commercially. A commercial
future for perovskite appears more likely than f or sphene because
perovskite is richer in TiO2 and has only calcium as its main
troublesome impurity. Sphene, on the other hand, contains as major
components, calcium and silica, both problem impuritie s.
183
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184
TABLE 44 World Ilmenite Resource pa (million short tons of contained
t itanium) b
Lo cation
ReservesOtherTotal
North America
Canada 4 93786
Co sta Rica -11
United States 1779c9 6
Subtotal 66117180
South America
Argentina -11
Bra zi 1 123
Uruguay -22
Subtotal 156
Europe
Pi eland 314
Norway 4054 5
Soviet Union 41620
Subtotal 47226 9
Af rice
Ma zambique -1313
Senegal -22
South Af rice, Republic of 33117150
Tanzani a -44
Egypt 1910
Upper Volta -44
Other -11
Subtotal 35150180
Asia
India S O
Indonesia
Malaysia
Sri Lanka 1
Other -
Subtotal 51
Oceania
80 130
1
1
1
1
2
135
An stralia 18 9 27
New Zealand ~ 7 7
Subtotal 18 16 34
World Total (rounded ~220 390 600
a
b
c
Resource data deriv . in consultation with the U.S. Geological
Survey .
Individual items may not add up to totals because of independent
rounding .
Includes perovskite deposits in Colorado.
Source: U . S . Bureau of Mines 1980 .
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185
TABLE 45 World Rutile Resources a ~ thousand short tons of contained
t itanium~b
Location
ReservesOtherTo tat
North America
Canada -200200
Mexico -2, 9002, 900
IJnited States 1,0007,6008,600
Subtotal1, 00010, 70011, 70 0
South America
BrazilE 60,00040,000100,000
Uruguay _-_ - _
Subtotal 60,00040,000100,000
Europe
Italy 2,7004,5007,200
USSR 1 6001, 5003, 100
Subtotal4,3006,00010,000
Af rice
Mozambique -1,2001,200
Senegal -100100
Si erra Le one 1 ,80016, 000IS, 000
South Af rice, Republic of3, 2003003, 500
South-Wes t Af rice - d d
Subtotal 5,000 18, 000 22, 800
Asia
India 5,000 12,000 17,000
Sri Lanka 200 100 300
Subtotal 5,000 12,000 17, 000
Oceania
Australia 6~000 1,600 7,600
World Total (rounded) 81,000 88,000 169,000
a Resource data derived in consultation with the U.S. Geological Survey
b Individual items may not add up to totals because of independent
rounding.
c Mainly anatase deposits.
d Le ss than 50,000 tons.
Source: U . S . Bureau of Mines 1980
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TABLE 46 U. S. Titanium Resources a (thousand short tons of contained
t itanium~b
Reserves Other
State Ilmenite Rutile IL~neniteERutile
Ari zone
Arkansas
Calif orni
Colorado
Florida
Georgia
Id aho
Minnesota
New Jersey
New Mexico
New York
North Carolina
Oklahoma
3,500
2 9, ooo
2, 100
300
1,100
11,000
5,000
500
7,100 - 12,000
500
2,200
1,200
900
1,800
5,600 600
1, 400 300
1,700
Oregon
South Caro line
Tennes see
Utah
Virginia
Wa shing ton
Wyoming
Other States -- -
800 100
3, 000
300
4,300
300
~-
Total
Ilmenit e Rutile
2,700 --2,700
300 - - -300
100
800
100
100
100
200
2,600
600
3,000
300
4,300
300
3,500
29,000100
7,7001,400
1, 7 00400
1,100
11,000
6,700
500
19, 100
500
2,200
1, 200
900
2, 600
100
100
300
2,600
600
Total (rounded) 17,000 1,000 79,000 7,600 96,000 8,600
a Resource data derived in consultation with the U.S. Geological Survey.
b Individual i tems may not add up to totals because of independent
rounding .
c Includes perovskite deposits in Colorado.
Source: U . S . Bureau of Mines, 1980.
Ti tanium in West Coast Sand-Gravel, Gold Placer and
Silica-Clay Operations
Po ssible recovery of heavy minerals was investigated by the U. S .
Bureau of Mines in 36 sand samples taken at various plant sites in
northern California (Games 1919~. TiO2 analysis of the samples and
beneficiated product were converted to percent ilmenite. Only 0.05
percent ilmenite or less was found in most of the samples; a f ew
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contained 0.1 to 0.5 percent ilmenite and one, a silica-clay operation at
lone, Amador County, California, contained about 20 percent ilmenite in
its tailings. A heavy minerals concentrate made on spirals was
fractionated magnetically to yield a TiO2 product of 63.5 percent grade
and about 68 percent recovery. The operation is on a leased site and
data on the tonnage of the plant tailings has been withheld pending
resolution of the tailings ownership.
A subsequent sampling survey by the U.S. Bureau of Mines (Gomes 1980)
of sand and gravel operations in central and southern Calif ornia showed
two sands containing O. .6 to 1.2 percent ilmenite in the northern San
Joaquin Valley, one containing 0.6 percent ilmenite in the Los Angeles
area, and two containing 0.6 to 0.8 percent ilmenite in the San Diego
area . A benef iciation test on the O. .6 percent ilmenite sand f ram the Lo s
Angeles area, using spirals and low intensity and high intensity magnetic
equipment, yielded a TiO2 concentrate that analyzed 43 percent TiO2
and 48 percent Fe2O3. Further test work might show that processing
the ilmenite-bearing sands to produce a crude heavy minerals product at
individual operations followed by centralized processing to recovery
magnetite, ilmenite, gold, platinum, and even thorium-uranium may be
worthwhile ~ Come s 1980) .
A survey of sand and gravel deposits in Oregon and Washington
(Martinez et al . 1981) showed 2.5 percent ilmenite in a sample from
Moclips Beach, Washington. Beneficiation tests yielded a product
analyzing 47 percent TiO2 and 3 percent Cr2O3. If the deposit is
large enough to be of potential interest as an ilmenite source, tests to
remove the Cr2O3 might be warranted.
REFERENCE S
Come s , J . M., G. M. Martinez , and M. M. Wong . 197 9. Recovery Byproduc t
Heavy Minerals from Sand and Gravel, Placer Gold, and Industrial
Mineral Operations, USBM RI 8366:15.
Gomes, J. M., G. M. Marti nez, and M. M. Wong . 1980. Recovery of
Byproduct Heavy Minerals from Sand and Gravel Operations in Central
and Southern California, USBM RI 8471:20.
Martinez , G. M., J. M. Gomes, and M. M. Wong . 1981. Recovery of
By-product Heavy Minerals f ram Sand and Gravel Operations in Oregon
and Washington. Report of Investigation 856 3. Washington, I) . C . U . S .
Bureau of Mines.
U. S. Bureau of Mines. 1980. Mineral Facts and Problems. Washington,
~ . C .: U. S . Government Printing Of f ice .
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Representative terms from entire chapter:
heavy minerals