Three-dimensional deep geoelectric model of the Tarasivka structure of the Golovanivsk suture zone

Journal Title: Геофизический журнал - Year 2018, Vol 40, Issue 2

Abstract

In 2017 the field simultaneous areal measurements of the external low-frequency natural electromagnetic field of the Earth and the construction of a three-dimensional deep resistivity distribution in the crust of the Tarasivka structure (48032' N, 30037' E) were performed in the central part of the Yatran Block of the Golovanivsk suture zone. The analysis of experimental data (the curves of deep magnetotelluric sounding for a period of 10—10000 s and the complex induction parameters for periods of 20—6900 s) indicates a complex three-dimensional situation, which involves the presence of a nearsurface and possibly deep conductivity anomalies. According to the results of three-dimensional modeling, the Tarasivka structure is fragmentarily manifested as a low resistivity, the conductive zones with different resistivity cross it in a sublatitudinal direction, in which the lowest values from 10 Ohm·m in the south to 100 Ohm·m in the north are in its contour. In the vertical section it can be represented in as several layers: the first one is the conductor with ρ=10ч250 Ohm·m — from the surface to 10 m (south of 48030ў) to 100 m (north of 48030ў), most likely linked not only with high electrical conductivity of surface sediment deposits, but also with the zones of disintegration of rocks of the basement; the second one is a high resistivity layer with ρ=10000 Ohm·m — from 100 m to 2 km, possibly it is represented by the uniform non-differentiated thickness; the third layer is the electrical conductor with ρ=10ч250 Ohm∙m from 2—3 km to 10 km, probably linked with the special composition of the earth’s crust at these depths (graphitization, sulfidization, etc.) or fluidization of different origins, more often it is considered according to the modern data that the nature of the conductive anomalies is the result of the joint influence of the electron and ion types of electrical conductivity.

Authors and Affiliations

T. K. Burakhovich, V. A. Ilyenko, A. M. Kushnir, B. I. Shirkov

Keywords

Related Articles

Geophysical model of the mantle ore-forming system

The paper deals with a generalized geophysical model of the mantle ore-forming system that covers three main parts: a) the area of origin of the ore substance; b) its transportation zone and c) the area of concentrated o...

Petrophysical parameters of rocks of the Visean stage (Lokhvytsky zone of the Dnieper-Donets Depression)

The results of complex investigations of petrophysical properties of the Visean rocks from wells in Lokhvytsky zone of the DDD (sandstones and siltstones from depths 5060―5600 m and limestones from depths 5960―6200 m) ar...

To the problem of the origin of the Bug series rocks

The age of the Bug series rocks is an object for discussion. Isotopic methods do not give a distinct answer, because in the same outcrop, the same sample and even in the same crystal of zircon several dates of formation...

Identification of hard-to-recover reserves of Ugra oil

More than 70 % of the reserves of Yugra oil fields, which are in development and at various stages of study, are classified as hard-to-recover (HTR). Active involvement in the development of HTR will prevent the decline...

Simultaneous seismic inversion to identify prospective areas in carbonate rocks of the southeastern part of the West Siberian Platform

This paper focuses on the description of a technology and results of identifying and mapping areas in Devonian carbonate rocks prospective for hydrocarbons and associated with increased fracture-cavern porosity in the so...

Download PDF file
  • EP ID EP282073
  • DOI 10.24028/gzh.0203-3100.v40i2.2018.128934
  • Views 66
  • Downloads 0

How To Cite

T. K. Burakhovich, V. A. Ilyenko, A. M. Kushnir, B. I. Shirkov (2018). Three-dimensional deep geoelectric model of the Tarasivka structure of the Golovanivsk suture zone. Геофизический журнал, 40(2), 108-122. https://europub.co.uk/articles/-A-282073