Bayannaoer chemicals non-metallic mineral pyrite, phosphate, salt, Glauber's salt, potassium rock, alunite, fertilizer use serpentinite, arsenic, barite. There are 28 mineral deposits, including 8 large deposits, 4 medium-sized deposits, 4 small deposits, and the rest are mines. Sulfur, iron ore is the alliance of the most important advantages of mineral in the country also occupies an important position made, there are large deposits of pyrite is at 6, 2 medium-sized deposits. (The pyrite deposit has been discussed in non-ferrous metals)
1. Phosphate ore and phosphate rock are the shortage minerals in Bayannaoer City. It is known that there are 6 phosphate mines, including 1 medium-sized deposit, which is the carbon kiln mouth of Urad Rear Banner, and 2 small deposits, which are Urad Middle Banner. West Daqi, Hou Daqi, the rest are mines. Finding reserves: The reserves of the upper balance sheet: 363 thousand tons, the basic reserves: 725 kilotons. The amount of resources is 764 thousand tons. Resource reserves: 1489 thousand tons. Unbalanced table resource reserves: 5,781,000 tons. It accounts for 100% of the autonomous region and is a poor ore with P2O 55%-11%. The deposit is due to sedimentary metamorphism. The mine is in the Yuan Dynasty and the Baiyun Obo Group.
2, Glauber's salt, only one small deposit was identified in the territory, which is the Urad Rear Banner Bayin Suimu Sumu Dabu Sushen. It is a modern lake phase chemical deposition type. The lake is 1.1 kilometers long and 0.5 kilometers wide. Chemical deposits include: thenardite, potassium and salt. The Glauberite Mine is 700 meters long, 1000-180 meters wide and 0.79-3.84 meters thick. The ore grade: Glauber's salt (Na2SO4) is 42.10%, and the balance of the old woman's balance table is found: 280 kilotons.
3, salt (pool salt, Bayan Muer City, there are salt (chi salt) in the production of 5, are mine points, for the Urad Front Banner Yong Donghaizi (Lao Lundan), Xishanzui Yanhaizi (Nanda Dam), Dongpuchi, Shashibao, Ulaitetehouqi Dabusu 嘎Nuoer. The genesis of the deposit belongs to the evaporative sedimentary deposit.
4. Mingshi Stone, there are only 3 alum stone deposits in Bayannaoer City, which is the former Uttar Pradesh, the Shima Pile, and the Sulun Township Molun River. The genetic type of the deposit is weathered and leached. The alum stone is produced in the carbonaceous slate of the Agulugou Formation of the Zhaertai Group in the Proterozoic. It is distributed in a fine vein. The alum stone is acicular and fibrous.
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