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Articles by Irina N. Plotnikova
Total Records ( 2 ) for Irina N. Plotnikova
  Irina N. Plotnikova
  The base platform areas geological structure study represents the composite and actual issues, solution of which is directed on knowledge of development and evolution history of crust and sedimentary cover of the studied territories. Exhaustive ideas of the base geological structure make the basis of the formation process exact comprehension for sedimentary cover and regularities of mineral deposits placement in it, first of all, oil and gas. In study results of crystal base study of the Volga-Kamsky anteclise central part are considered. Implementation of the deep drilling long-term program allowed to reveal the numerous loosened zones which are characterized by water saturation in crystal base solids. The content of the dissolved hydro-carbonic gases in water as well as oil row bitumoid presence in the loosened zones specifies that through the crystal base there was a migration of oil hydro-carbons, the deep fluids containing hydro-carbons, gases. Solids of the base represent a great interest from the oil fields origin point of view and also in aspect of deep fluid systems migration. Geo-dynamic activity of the loosened zones shows the modern processes of fluid migration and their influence on oil field formation in a sedimentary cover.
  Raphael L. Ibragimov and Irina N. Plotnikova
  Recently, the solids of Archaean-Proterozoic age attract more and more attention of oil geologists, especially in connection with possible prospects of oil-bearing capacity. In the Tatarstan Republic territory for >20 years within the program of deep structure study for the express deep wells base drilling which allowed to receive new unique information on crystal base structure and prospects of its oil and gas content was carried out. It should be noted that all deep parametrical, explorative and operational wells of Tatarstan which in a varying degree were objects of KF collectors study can be divided into four categories conditionall. The wells which opened crystal solids of the Precambrian on the maximal depth over 3000 m. The wells which opened crystal solids of the Precambrian on the considerable depth from 200-3000 m. The wells which opened crystal solids of the Precambrian on depth from 50-200 m. The wells which opened crystal solids of the Precambrian on depth <50 m. The third and fourth wells categories are the most numerous, total more than one thousand wells drilled since the base opening in the middle of the last century.
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