Standard

Комплексная электропроводность кимберлитовых пород. / Емельянов, В. И.; Титов, К. В.; Ревил, А.

Engineering and Mining Geophysics 2020. European Association of Geoscientists and Engineers, 2020. p. 1-6 (Engineering and Mining Geophysics 2020).

Research output: Chapter in Book/Report/Conference proceedingConference contributionResearchpeer-review

Harvard

Емельянов, ВИ, Титов, КВ & Ревил, А 2020, Комплексная электропроводность кимберлитовых пород. in Engineering and Mining Geophysics 2020. Engineering and Mining Geophysics 2020, European Association of Geoscientists and Engineers, pp. 1-6, Engineering and Mining Geophysics 2020, Perm, Russian Federation, 14/09/20. https://doi.org/10.3997/2214-4609.202051102

APA

Емельянов, В. И., Титов, К. В., & Ревил, А. (2020). Комплексная электропроводность кимберлитовых пород. In Engineering and Mining Geophysics 2020 (pp. 1-6). (Engineering and Mining Geophysics 2020). European Association of Geoscientists and Engineers. https://doi.org/10.3997/2214-4609.202051102

Vancouver

Емельянов ВИ, Титов КВ, Ревил А. Комплексная электропроводность кимберлитовых пород. In Engineering and Mining Geophysics 2020. European Association of Geoscientists and Engineers. 2020. p. 1-6. (Engineering and Mining Geophysics 2020). https://doi.org/10.3997/2214-4609.202051102

Author

Емельянов, В. И. ; Титов, К. В. ; Ревил, А. / Комплексная электропроводность кимберлитовых пород. Engineering and Mining Geophysics 2020. European Association of Geoscientists and Engineers, 2020. pp. 1-6 (Engineering and Mining Geophysics 2020).

BibTeX

@inproceedings{916b0336aa8945458893c1f3802653cb,
title = "Комплексная электропроводность кимберлитовых пород",
abstract = "Kimberlites are the main sources of diamonds. In field geophysics kimberlite pipes are characterized by anomalies of low resistivity. However, the reason for high electrical conductivity is not clear. We have carried out multisalinity experiments with two kimberlite samples (autolitic and xenotuffisitic breccia) from Arkhangelsk region (Lomonosova Deposit). Samples were saturated with brines of different electrical conductivity values (from 0.01 to 3.77 S/m). Complex electrical conductivity was measured with SIP FUCHS-III instrument in the frequency range from 1.43 mHz to 20 kHz. We found the bulk conductivity of sample is larger than that of the pore water (at the brine electrical conductivity range typical for fresh water). The quadrature conductivity values at 1.46 Hz are larger than that typically obtained for e.g., magmatic rocks and sandstones. We attribute this complex conductivity behavior to the surface conductivity influence. Furthermore, our kimberlite samples have a high values of cation-exchange capacity (CEC). It can be explained by the presence of smectites in mineral composition.",
author = "Емельянов, {В. И.} and Титов, {К. В.} and А. Ревил",
note = "Publisher Copyright: {\textcopyright} Engineering and Mining Geophysics 2020. Copyright: Copyright 2021 Elsevier B.V., All rights reserved.; Engineering and Mining Geophysics 2020 ; Conference date: 14-09-2020 Through 18-09-2020",
year = "2020",
month = sep,
day = "14",
doi = "10.3997/2214-4609.202051102",
language = "русский",
series = "Engineering and Mining Geophysics 2020",
publisher = "European Association of Geoscientists and Engineers",
pages = "1--6",
booktitle = "Engineering and Mining Geophysics 2020",
address = "Нидерланды",

}

RIS

TY - GEN

T1 - Комплексная электропроводность кимберлитовых пород

AU - Емельянов, В. И.

AU - Титов, К. В.

AU - Ревил, А.

N1 - Publisher Copyright: © Engineering and Mining Geophysics 2020. Copyright: Copyright 2021 Elsevier B.V., All rights reserved.

PY - 2020/9/14

Y1 - 2020/9/14

N2 - Kimberlites are the main sources of diamonds. In field geophysics kimberlite pipes are characterized by anomalies of low resistivity. However, the reason for high electrical conductivity is not clear. We have carried out multisalinity experiments with two kimberlite samples (autolitic and xenotuffisitic breccia) from Arkhangelsk region (Lomonosova Deposit). Samples were saturated with brines of different electrical conductivity values (from 0.01 to 3.77 S/m). Complex electrical conductivity was measured with SIP FUCHS-III instrument in the frequency range from 1.43 mHz to 20 kHz. We found the bulk conductivity of sample is larger than that of the pore water (at the brine electrical conductivity range typical for fresh water). The quadrature conductivity values at 1.46 Hz are larger than that typically obtained for e.g., magmatic rocks and sandstones. We attribute this complex conductivity behavior to the surface conductivity influence. Furthermore, our kimberlite samples have a high values of cation-exchange capacity (CEC). It can be explained by the presence of smectites in mineral composition.

AB - Kimberlites are the main sources of diamonds. In field geophysics kimberlite pipes are characterized by anomalies of low resistivity. However, the reason for high electrical conductivity is not clear. We have carried out multisalinity experiments with two kimberlite samples (autolitic and xenotuffisitic breccia) from Arkhangelsk region (Lomonosova Deposit). Samples were saturated with brines of different electrical conductivity values (from 0.01 to 3.77 S/m). Complex electrical conductivity was measured with SIP FUCHS-III instrument in the frequency range from 1.43 mHz to 20 kHz. We found the bulk conductivity of sample is larger than that of the pore water (at the brine electrical conductivity range typical for fresh water). The quadrature conductivity values at 1.46 Hz are larger than that typically obtained for e.g., magmatic rocks and sandstones. We attribute this complex conductivity behavior to the surface conductivity influence. Furthermore, our kimberlite samples have a high values of cation-exchange capacity (CEC). It can be explained by the presence of smectites in mineral composition.

UR - http://www.scopus.com/inward/record.url?scp=85099680577&partnerID=8YFLogxK

U2 - 10.3997/2214-4609.202051102

DO - 10.3997/2214-4609.202051102

M3 - статья в сборнике материалов конференции

AN - SCOPUS:85099680577

T3 - Engineering and Mining Geophysics 2020

SP - 1

EP - 6

BT - Engineering and Mining Geophysics 2020

PB - European Association of Geoscientists and Engineers

T2 - Engineering and Mining Geophysics 2020

Y2 - 14 September 2020 through 18 September 2020

ER -

ID: 74982592