Lithological and X-ray phase analysis of clay deposits of the Lower Cretaceous of the Northwestern Caucasus allowed us to establish the conditions of their formation and the sources of erosion of clastic material. It has been established that the studied sediments were formed in normal marine relatively deep-sea conditions of the shelf. The clays of the Lower Cretaceous are characterized as rocks with high conservation properties capable of ensuring the safety of not only oil deposits, but also gaseous hydrocarbons.
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Yakovishin et al. (2024) studied this question.
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