Comparative Analysis of Oil-Saturated Fractured Reservoirs - Bazhenites Clays of Western Siberia and Khadumites of Eastern Caucasus

R. S. Dudaev, A. Elzhaev, S.S.-A. Gacaeva
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Abstract

The rocks of clay natural reservoirs present particular interest. On the one hand, they attract the attention of scientists from the point of view of oil content (they are enriched to a large extent with organic material), on the other hand from the point of view of accumulation of radioactive elements, as it is indicated by high radioactivity. In this regard, the article touches upon the issue of the relation of these factors. On the territory of the Russian Federation, such rocks are represented by the Jurassic bazhenites of Western Siberia and the Oligocene khadumites of the Eastern Caucasus. The article presents the peculiarities of the clay reservoirs of Western Siberia and Eastern Caucasus, a detailed description of the fractures of various generations, and the issues of reservoir capacity. A comparative analysis of the oilsaturated bazhenites of Western Siberia and the khadumites of Eastern Caucasus was carried out. The dependence of reservoir formation on the distribution of radioactive elements in the section
油饱和裂缝性储层——西伯利亚西部巴氏岩粘土与东高加索哈杜姆岩粘土对比分析
粘土天然储层的岩石表现出特别的兴趣。一方面,它们从含油量的角度引起科学家的注意(它们在很大程度上富含有机物),另一方面,从放射性元素的积累的角度引起科学家的注意,因为它具有高放射性。对此,本文就这些因素之间的关系问题进行了探讨。在俄罗斯联邦境内,这类岩石的代表是西伯利亚西部的侏罗纪巴氏岩和东高加索渐新世的哈杜姆岩。本文介绍了西伯利亚西部和东高加索地区粘土储层的特点,详细描述了各代裂缝,以及储层容量问题。对西伯利亚西部的含油bazhenites与东高加索的khadumites进行了对比分析。储层的形成与剖面中放射性元素分布的关系
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