GEOLOGICAL STRUCTURE PECULIARITIES OF LAYER BV<sub>10</sub><sup>1-2</sup> LOCAL CLINOFORMS OF SAMOTLOR FIELD
Layer BV<sub>10</sub><sup>1-2</sup>clinoform structure of Samotlor field is considered in the present article. New layer correlation with account for obliquely laminated rock location resulted in releasing of nine local bodies with common incline into south-eastern direction.