The correlation model of the main bondaries in the lithosphere section of the arch part of the Voronezh antecline

Authors

  • Александр Иванович Трегуб Voronezh State University image/svg+xml
  • Людмила Ивановна Надежка Voronezh State University image/svg+xml
  • Ирина Трофимовна Ежова Voronezh State University image/svg+xml

DOI:

https://doi.org/10.17308/geology.2018.1/1450

Keywords:

correlation model, Earth surface, lithosphere, Voronezh antecline

Abstract

Statistical analysis of the morphometric data relations with the main sections of the lithosphere was carried out according to the seismic profile Gubkin – Zherdevka. According to the results correlation analysis evaluated the statistical relationship between the morphometry of the earth`s surface and seismic boundaries: the boundary of Conrad, Mohorovichich`s boundary and the boundary of the transition layer. For megablock KMA linear relationship of the earth`s surface morphometry is determined only with the Conrad boundary. For Khopersky megablock of the only border Mohorovichich`s. For Ljsevskaya suture zone of dependence exists with major borders. These features are likely to be associated with different formation history of the basement blocks.

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Author Biographies

  • Александр Иванович Трегуб, Voronezh State University

    Doctor of Geological and Mineralogical Sciences, Professor of the General Geology and Geodynamics Department

  • Людмила Ивановна Надежка, Voronezh State University

    Head of the Tarkov Laboratory of deep Structure, Geodinamik and Seismic monitoring Voronezh Crystalline Massif FITS EGS RAS

  • Ирина Трофимовна Ежова, Voronezh State University

    Senior Researcher of a Tarkov Laboratory of deep structure, geodinamik and seismic monitoring Voronezh Crystalline Massif FITS EGS RAS

References

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Published

2017-11-08

Issue

Section

Geophysics

How to Cite

The correlation model of the main bondaries in the lithosphere section of the arch part of the Voronezh antecline. (2017). Proceedings of Voronezh State University. Series: Geology, 1, 121-126. https://doi.org/10.17308/geology.2018.1/1450

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