For the development of the economy, it was necessary to create a mineral-raw material base. This issue has been solved in sovets some time, especially in 1940-90. Development and utilization of mineral resources and in what follows we will lift the economy. Natural resources in Kyrgyzstan are mainly divided into four major groups: metals, nonmetals, energy resources, and groundwater.
BLACK
Iron. On the territory of Kyrgyzstan have dozens Xia deposits of iron, but they are still poorly understood. Only on the field at holes (Kadamjai district) were drilling, on the other – cal surface geological studies.
The field Bala Chychkan (exposed at the foot of the Talas Ridge, 30 km east of Talas, 5 km south-east of the village of Bazar-Chat). Mineralization is confined to nitam pyroxene. The main ore mineral – titanium-magnetite, in a rum-contained industrial concentration of iron, titanium, vanadium and cobalt that. Estimated reserves of iron on the C2 category 535 377 tonnes and the mine may be practiced open pit.
Zhetimskoe field (Naryn district, 60 km east of the town of Naryn, the northern slopes of the ridge Zhetimskogo, opened in 1956). The length of the iron pool 70 km, width of 10 km. It found six separate GOVERNMENTAL iron ore deposits (sites). Hundreds of lenticular and tabular ore bodies in leg of dark gray and green shales. The ores are mainly composed of hematite and magnetite, capacity 10-20 tons of ore bodies, this is no bad examples. The iron content in the ore 15,4-46,3%. The field is studied only from the surface. Total iron ore reserves of category C2 – 5.5 billion tons (iron – 1.74 billion tons).
The deposit is located in the Nadir Kadamjai borough, in the west. Ohna Valley, opened in 1931. The deposit was explored to a depth of 348 meters Mineralization is confined to the northern. and the south. contacts of the gabbro-ultramafic intrusive sion, so marked North. and South. ore zones. In these areas lie 15 ore bodies, and their length of 50-1310 m, thickness 1.2 – 6.1 m North. zone consists mainly of heme Titova ore, and the South. – Magnetite. Total reserves of iron ore 2.423 million tonnes (Mt of iron -1.019) iron content in the ore – 42.0%.
The deposit is located in Gava Ala-Buka district, on the watershed pp. Pressed-Giz-Apricot and Ortho-Suu. Magnetite ores occur in skarns at the contact between limestone and effective fuzivov. The field plate 11 is known and lenticular ore bodies, and their ABILITY of extended 40-150 m, thickness 3-35 m, developed to a depth of 50-150 m iron content in the ore is 38.8%, estimated reserves 2.576 million tons ( Iron – 1.0 million tons).
The deposit is located in the Lower Kemin Kemin district, in the upper reaches of the River. Kozhakmat, a left tributary of the river. Chon-Kemin. Mineralization is confined to the limestone at the contact between granite and siltstone. In the limestone areas of tectonic fractures occur five ore bodies, and their length of 5-100 m, the cardinality of – 5-15 m. The ores are composed predominantly but magnetite. Estimated reserves of iron to a depth of 100 m – 2.4 million tons, the content of the jelly in the ore 20,0-51,8%.
In Kyrgyzstan, there are two large iron ore deposits: Bala Chychkan and Zhetim. They can be used in future mineral syr Eve base of ferrous metallurgy in the republic. In small fields Nadir, Gava, Lower Kemin may construct small steel plants as They are located in an economically developed areas.
Manganese. The republic found only a few minor occurrences of manganese. They count exceeds 20, but the most valuable of them – 4. These rudoproyavlen Notices are not well understood. The manganese content in the ores is negligible. Ore occurrence to a p-and n A m and is located in the Suzak district, 50 km north-west of Jalal-Abad, in the valley. Kara-Alma. Ore occurrence consists of a 2-GOVERNMENTAL ore bodies: the length of one of them 300 m, thickness 0.4-0.5 m ore reserves of 485.7 thousand, 6.0% manganese content, the reserves – 29.1 thousand And that ore occurrence p h a n s is szyrts Ton district, on the left side of p. Arch ly sat down. Zhetimskogo slope of the ridge. Orient the gauge ore reserves to a depth of 100 tons – 2100 tons, the average content of manganese in the ore is 10% stocks – from 210 thousand. Ore occurrence and the p K a – K s r l a is in Aksy district of the Jalal-Abad, 20 kilometers north-west of Tash-Kemur, in the mountains Bozbey-Too. At $ 3 rudoproyavl struction site. Indicative of the ore passes to a depth of 100 m – 1728 tons, the average manganese content of 14.4%, the reserves – by 248.8 thousand. Ore occurrence of the T with a p is Tong district, 25 km south of Avtodor w Balykchy-Karakol. Width of the tungsten-manganese mineralization can reach 100 m, length at intervals of 1.8 km. In total 10 ore bodies, of which three are relatively large and relatively better known, their average length – 200 m, capacity – 0,55-7,75 m Roughly a matter of ore reserves in these three ore bodies – 1333.4 thousand from, the average content of manganese – 2.58% stocks – from 31.4 thousand. In addition to manganese in the ore contains a small amount of tungsten Fram.
In a n and g and h. Kyrgyzstan has registered dozens of Wana deposits and occurrences. Of these, as cost-effective for osvoe of, we can distinguish two ore deposits and one manifestation.
Sarah-Xia Zhazskoe field is in the Ak-Suu district of Issyk-Kelskoy area on the right side of p. Sary-Jaz. Uranium-molybdenum-vanadium mineralization is confined to a uglis-siliceous shales. The deposit of 5 um am ore sites in the square, a length of 10 km. At those sites identified eight GOVERNMENTAL ore bodies, the length of 300-2700 m, is powerful Stu 1,27-9,2 m Estimated ore reserves at 5 sites in the depths of 100-700 m in the categories C1 C2 up 21,819 tons, the average with the content of V 2 O 5 – 0.34%, the reserves – 74.6 thousand tons (total estimated reserves 112.8 thousand tons). In addition, Ore, together with vanadium, are contained: uranium (mean – 0.022%) and molybdenum (0.04%).
The ball on the field and H-s h a a n (nye given in the Hardware) are the major passes of four components (iron, titanium, vanadium, cobalt). The average metal content in the ore is low (iron – 16.7, vanadium – 0.08 Titanium – 0.73%).
Ore occurrence is in the lower Kurmenty szyrts Ton, in the mountains Zhetim-Bel, in the basin. Archaly. Vanadium can Libdeh-uranium mineralization in the concen Wang carbonaceous siliceous shales. Identified two ore body length of 60 and 80 m, the cardinality of 2 m have been estimated 60 kg of V 2 O 5 with an average grade of 0.23%. The average content of uranium and molybdenum – 0.02%.