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This research identifies sedimentation settings of Lower Cretaceous (Aptian-Albian) terrigenous sediments of the North Caspian, which are oil and gas reservoirs. These rocks are characterized by irregular distri- bution of pelitic and silty fractions, which leads to ambiguous results of petrophysical analyses. In order to correctly interpret the geophysical data, a detailed lithologic analysis of the rocks was carried out. In the studied area in the Early Cretaceous time marine conditions prevailed: coastal, shallow-marine, relatively shallow shelf lithofacies with signs of active hydrodynamics, as well as relatively deep-water shelf lithofacies of low hydrodynamics. The study of sections reveals a change from shallow-water sediments to deeper-water sediments and vice versa, which allows us to conclude that the sea level fluctuates periodically. Lithologic analysis also showed the predominance of shallow-water and coastal sediments in the Aptian time and deeper-water, shelf sediments in the Albian time. Consequently, we can assume the presence of local sea transgression in this study area during the Lower Cretaceous.
Churkina et al. (Tue,) studied this question.
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