BGV Titanium
Brochure
with detailed info about deposit
geology, mineralization. reserves,
permit and mining technology:
Key Points:
- Deposit is located in the metasomatic Suschano-Perzhanska zone.
- According to the studies two ore zones have been identified with content of titanium dioxide 5,5 and 7.0%.
- Ores enrichment has been studied during small-scale technological test.
- "Titan-Apatitova Group LLC" acquired a special permit for industrial development and subsequent extraction for 5 years.
Titanium and its alloys are widely
used because of their high
mechanical strength, which is
maintained at high temperatures, corrosion resistance, heat
resistance, low density and other
useful properties
Fields of application:
- Πerospace
- Marine ship building
- Manufacturing of equipment operating in aggressive environments
- Parts of devices operating at high temperatures
YURIEVSKOYE TITANIUM-APATITE ORE DEPOSIT
Zhytomyr Region, Ukraine
Yurievskoye deposit is located in
the Zhytomyr
region. Deposit area is connected
with the district center by asphalted roads.
The railway KyivBrest passes Olevsk.
In geostructural terms, the Yurievskoye deposit of titanium-apatite ores is located within the central part of the Sushchano-Perzhanska tectonic zone and is confined to the rock intrusion of the same name, which was formed at the final stages of the Korosten complex.
In geostructural terms, the Yurievskoye deposit of titanium-apatite ores is located within the central part of the Sushchano-Perzhanska tectonic zone and is confined to the rock intrusion of the same name, which was formed at the final stages of the Korosten complex.
The Yurievsky intrusion is almost
completely covered with a thinwalled
thickness (to the first meters,
sometimes 10-15 m in the
northern part)
of sandy-clay rocks, mainly of
fluvio-glacial genesis. On
crystalline rocks
the weathering crust occurs with
thickness of 0,0-16,0 m.
The content of titanium dioxide (TiO2) in the Yurievskaya intrusion de= pends on the angle of the rock layers fall. The richest ores are confined to the central and northern parts of the deposit and are concentrated mainly on the lying side of the ore zone. Liquation apatite-ilmenite ore bodies are confined to the lying side of the array. The maximum content of ilmenite and titanomagnetite is recorded in melanocratic varieties.
According to the structural and petrographic studies two ore zones have been identified with content of titanium dioxide 5,5 and 7.0%.
The content of titanium dioxide (TiO2) in the Yurievskaya intrusion de= pends on the angle of the rock layers fall. The richest ores are confined to the central and northern parts of the deposit and are concentrated mainly on the lying side of the ore zone. Liquation apatite-ilmenite ore bodies are confined to the lying side of the array. The maximum content of ilmenite and titanomagnetite is recorded in melanocratic varieties.
According to the structural and petrographic studies two ore zones have been identified with content of titanium dioxide 5,5 and 7.0%.
It has been established that the
main rock-forming minerals of
titanium
and phosphorus in ores are
ilmenite and apatite. Accordingly,
85.3-
92.3% of the total amount of TiO2
and 61.6-86.6% of the total
amount
of P2O5 present in the ores are
bound to them.
Other useful components are
scattered in rock-forming and
other ore
minerals (titanomagnetite,
magnetite).
Enrichment of ores can be carried out according to the schemes developed for the Stremigorod apatite-ilmenite deposit of Volyn titanic province and tested by the USSR DKZ. The material composition and enrichment of ores within the Yurievskoye deposit is studied basing on the materials of a small-scale technological test.
Enrichment of ores can be carried out according to the schemes developed for the Stremigorod apatite-ilmenite deposit of Volyn titanic province and tested by the USSR DKZ. The material composition and enrichment of ores within the Yurievskoye deposit is studied basing on the materials of a small-scale technological test.