Model of Overthrust of Korotaikha Depression

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We crafted a 3D model of surfaces in southeastern areas where overthrust has occurred, specifically in Sub-Pay-Khoy – Sub-Southern Novaya Zemlya foredeep and Pay-Khoy-Novaya Zemlya folded systems based on past [2] and current [1, 3] data. The model accurately depicts the area's complex structure, including detachment surface development and fault plane relationships in three-dimensional space. The lower boundary of the model is defined by the detachment surface at the base of Korotaikha Depression's sedimentary cover. The southwestern border is marked by a Talota Thrust ramp, while the northeastern border is situated along Baydarata Suture. State Geological Map of Russia, Scale 1:1,000,000 (Third Generation), South Kara Series: R-41 (Amderma). VSEGEI. Yudin V.V. Orogeny in Northern Urals & Pay-Khoy. UIF Nauka, Ekaterinburg. 1994. Yudin V.V., Remizov D.N. A balanced geodynamic model on Polyarnouralsky transect profile. Materials XVI of the Geological congress of Komi Republic.