The Siyazan monocline is located in the Caspian-Guba oil-gas region and stretches for 90 km along the foothills of the South-Eastern Caucasus. This 800 m wide strip-shaped area is located between Zorat station and Karachay. It consists of areas with different structures according to the terrain. It stretches from Atacay to Kilkilay in the southeast with a coastal plain and low hills, while the North-West area passes through relatively high plains and forests. Wells are often drilled deep (about 1000 m long and more), equipped with uncemented, ready-made filter casing, and the entire unit is operated together. The upper part of the unit consists of oil-saturated chalk sediments, and the lower part consists of non-retentive (clay-sandy) rocks. As a result, only the upper part of the bed is exploited. The surface of the Siyazan monoclinal deposit has many water networks crossing it (Garachay, Caghajugchay, Valvalechay, Shabranchay, Kilkilachay, Atachay). The tributaries of these water bodies do not dry up even in the summer months. Ready-made filters are used in wells exploiting layers of chalk sediments located at an angle of 70–80o. Over time, irrigation in such wells occurs due to the opening of holes in the perforation interval to large distances and bottom water entering the well from lower wells.
Read full abstract