The analysis of a square distribution of conductivity factor in collectors of tolbachansky suite in a cross-cutting mass of field the tube «International»

Authors

  • Алексей Михайлович Янников Voronezh State University image/svg+xml

DOI:

https://doi.org/10.17308/geology.2019.2/1804

Keywords:

Nepsko-Botuobinsky anteklise, Mirninsky ledge, field of a tube, tolbachansky suite, elgyansky suite, marginal jointed collector, saturated brines, conductivity coefficient

Abstract

Hydrogeological and hydrogeochemical data on tolbachansky and elgyansky suites in near-tubular space of the radical diamond field «International» tube, belonging to a southwest part of the Ya-kutskoy kimberlite province located along the Vilyuysk-Markhinsky zone of breaks where the Mirninsky diamondiferous kimberlite field is revealed are taken as a basis of article. On the basis of basic data the hydrogeological characteristic of brines tolbachansky is given and elgyansky the analysis of data is twisted, carried out: in the first case on the basis of temporary regularity of an output, in the second –- on temporary regularities of the given decrease. Also, on the basis of a graphic-analytical method, on sites of the schedules answering to the near-tubular mode of filtration vulgar distribution of coefficient of con-ductivity in the okolotrubochny massif of the field a tube of «International» on the observation wells 1D, 2D, 3D, 5D, 6D, 7D, 9D, 12D drilled in underground excavations of the International mine on the horizon has been calculated. (-790) m.

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Author Biography

  • Алексей Михайлович Янников, Voronezh State University

    Senior hydrogeologist Vilyui GRE, postgraduate student of the Department of hydrogeology, engineering Geology and Geoecology Department

References

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Published

2018-11-01

Issue

Section

Brief Reports

How to Cite

The analysis of a square distribution of conductivity factor in collectors of tolbachansky suite in a cross-cutting mass of field the tube «International». (2018). Proceedings of Voronezh State University. Series: Geology, 2, 146-149. https://doi.org/10.17308/geology.2019.2/1804

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