The Altankhudag Almandine type of Garnet
deposit is located 1160 km south west from Ulaanbaatar,
160 km south from Gobi-Altai aimag (province), 7 km
south east from Tseel Soum (Figure1). GBM owns 100%
interest of Altankhudag license since 2005 and is conducting
exploration work. (Figure 1)
The deposit was first discovered in
1968 and since then, the prospecting work has been successfully
executed. In 1978-1986, “Zoos Goyol” state-owned plant
has been mining the deposit for jewelry products and
exported its poducts to then-called Czechoslvakia and
Hungary. (Figure 2)
In 1986-1988, an expedition headed by T.Namsrai,
successfully completed a prospecting in placer deposit
(report 4236) and found out that it has a reserve
of 38 tons of Garnet of B+C category including 832
kg of jewelry Almandine that accommodates industrial
requirement fully. Also the expedition made conclusion
that the reserve of the hard rock deposit will possibly
increase as it goe deeper. The Almandine occurs raisin-like
red, semi-transparent red coloured, flawless, right-shaped
crystal, with the size of more than 3mm, which attracts
so much interest in jewelry industry.
In 2006, GBM geologists visited site for exploration-evaluation
purpose in September to successfully complete a prospecting
in placer and hard rock deposits and estimated that
it has a placer reserve of 30 tons and a hard rock
reserve of 160 thousand tons of Garnet-Almandine of
C1 category. During the exploration trip there was
discovered unnamed occurence rich in (60-80%) of Garnet-Almandine
at the site (Figure 6).
Regarding the infrastructure of the deposit, a new
hydroelectric power station of Taishir will be opened
in 2007 and then, Tseel soum will be fully supplied
with reliable electricity. Also a regular Bichigt
border port at the Mongolian-Chinese border locates
and works at 170 km in southeast from the deposit.
The geological formation of the deposit sits at southern
area of Mongol-Altai mountain ranges and east part
of the Bichigt metamorphic series, and the Garnetized
metamorphic rock, which sits at the north of Bulgan
major fault creates a dyke-lenticular-shaped body
trending towards north-east. Garnetized body is composed
of various sheeting gniesses including biotite garnet,
biotite-mica garnet (70-80% garnet), garnet-bearing
quartz-feldspar-biotite-mica, biotite-amphibolite,
garnet-fibrolite (30-40% garnet) which basically forms
placer deposit (Figure 5).

(Figure 3).

(Figure 4).
The width of the body is 2-10 m,
length 400 m, trending is by 3X50’ and the dip dir
is 40-50/70-80 (Figure 2.3). Garnet occurs in different
sizes and the grain size ranges from 0.1-5mm, 5-10mm,
10-50mm and occasionally up to 100mm. The Garnet occurs
in transparent red, dark brown, brownish red, dark
purplish-red colour, in forms of right-shaped dodecahedrons,
round dodecahedrons, massive, detritus and modulus
7-7.8 hardness (Figure 7). The Altankhudag Garnet-Almandine
is very suitable for jewelry, sandblasting, textile
blasting (jeans so on), water filtration, concrete
floor finishingproduct, glass and tube plasting, water
jet cutting and for various other usages.
We are ready to collaborate
by everything subjects and participate with foreign
and local investors for interesting our Anar-Almendine
coalfield.

(Figure 5).

(Figure 6).

(Figure 7).

(Figure 6).

(Figure 6).