Teyruk oil field

The Teyruk oil field is one of the important oil fields in Russia. It was discovered in 1968 near the village Kinzebulatovo , Ishimbay district . This was a time when the ever-increasing global demand for oil was an important stimulus for the USSR, because the country survived at the expense of its natural wealth, and the production in the country was very bad - it was little quoted and practically nothing was exported for weapons . One of the most important works that the Soviet government paid attention to was the development of oil fields. Such an important object was the Teyruk oil field discovered and immediately explored in 1968.

This field is still operational and is operated by ANK Bashneft . However, over the long decades of exploitation, the reserves of the Teyruk deposit have become largely depleted ^[1] . Currently, this depletion of reserves has affected five oil fields in the Ishimbay district of the Republic of Bashkortostan (Teyruk, as well as: Allakayevskoye, Ishimbayskoye, Kusyapkulovskoye, Tsvetaevskoye). This is of concern to the State Employment Center of the Ishimbay district of the Republic of Bashkortostan - it is understandable, unemployment is threatening until recently successful deposit workers. ^[2] The city of Ishimbay and its settlements, as a matter of fact, grew up on the Bashkir oil-extracting and oil-refining industry: the settlement of geologists, where the building was temporary, gradually expanded, capital construction was carried out. To transport oil, the Ufa-Ishimbaevo railway branch was built, and an oil refinery was put into operation on the left bank of the Belaya River .

The coordinates of the field are 53 ° 17 ′ s. sh. 56 ° 16 ′ east. d.

Geologically located in the Shikhan-Ishimbay saddle ^[3] . The field gave the term "Teyruk type" for the dome-shaped folds of reefs in the southern part of the Pre-Ural marginal deflection ^[4] .

The reservoir horizon and its age differs by the Artinsko-Sakmar and Middle Carboniferous.

The Teyruk deposit differs from the others in that only there are sandy reservoirs in the Artinskaya stage ^[5] (Artinsky stage - with erosion. Limestone and dolomite are light gray, crystalline with interlayers of bluish-gray anhydrite ^[6] ).

The depth of the Artinsko-Sakmar horizon is 1021 meters, the total thickness of the reservoir is 49 m. The flow rate is 2.7 thousand m³ per day.

The depth of the Middle Carboniferous horizon is 1,138 meters, the total thickness of the reservoir is 140 m. The flow rate is 17 thousand m³ per day.

Murat Abdulkhakovich Kamaletdinov participated in the development of the field ^[7] .