Review of Processing and Interpretation of Self-Potential Anomalies: Transfer of Methodologies Developed in Magnetic Prospecting

The self-potential (SP) method is one of the most inexpensive and unsophisticated geophysical methods. However, its application is limited due to the absence of a reliable interpreting methodology for the complex geological-environmental conditions. To exclude disturbances appearing in the SP method...

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Main Author: Lev V. Eppelbaum
Format: Article
Language:English
Published: MDPI AG 2021-04-01
Series:Geosciences
Subjects:
Online Access:https://www.mdpi.com/2076-3263/11/5/194
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spelling doaj-6e225b327e964a6a9211085ce7789cc72021-04-29T23:07:55ZengMDPI AGGeosciences2076-32632021-04-011119419410.3390/geosciences11050194Review of Processing and Interpretation of Self-Potential Anomalies: Transfer of Methodologies Developed in Magnetic ProspectingLev V. Eppelbaum0Department of Geophysics, School of Earth Sciences, Faculty of Exact Sciences, Tel Aviv University, Ramat Aviv, Tel Aviv 6997801, IsraelThe self-potential (SP) method is one of the most inexpensive and unsophisticated geophysical methods. However, its application is limited due to the absence of a reliable interpreting methodology for the complex geological-environmental conditions. To exclude disturbances appearing in the SP method, a few ways for their removal (elimination) before quantitative analysis are presented. A brief review of the available interpretation methods is included. For the magnetic method of geophysical prospecting, special quantitative procedures applicable under complex physical-geological environments (oblique polarization, uneven terrain relief and unknown level of the normal field), have been developed. The detected common peculiarities between the magnetic and SP fields make it possible to apply the advanced procedures developed in magnetic prospecting to the SP method. Besides the reliable determination of the depth of anomalous targets, these methodologies enable the calculation of the corrections for non-horizontal SP observations and to determine the orientation of the polarization vector. For the classification of SP anomalies, is proposed to use a new parameter: the ‘self-potential moment’. The quantitative procedures (improved modifications of characteristic point, tangent techniques and the areal method) including the determination of the SP vector and SP moment, have been successfully tested on models and employed in real situations in mining, archaeological, environmental and technogenic geophysics. The obtained results indicate the effectiveness of the presented methodologies.https://www.mdpi.com/2076-3263/11/5/194quantitative analysiscomplex geological environmentsself-potential momentpolarization vectorore depositsarchaeological sites
collection DOAJ
language English
format Article
sources DOAJ
author Lev V. Eppelbaum
spellingShingle Lev V. Eppelbaum
Review of Processing and Interpretation of Self-Potential Anomalies: Transfer of Methodologies Developed in Magnetic Prospecting
Geosciences
quantitative analysis
complex geological environments
self-potential moment
polarization vector
ore deposits
archaeological sites
author_facet Lev V. Eppelbaum
author_sort Lev V. Eppelbaum
title Review of Processing and Interpretation of Self-Potential Anomalies: Transfer of Methodologies Developed in Magnetic Prospecting
title_short Review of Processing and Interpretation of Self-Potential Anomalies: Transfer of Methodologies Developed in Magnetic Prospecting
title_full Review of Processing and Interpretation of Self-Potential Anomalies: Transfer of Methodologies Developed in Magnetic Prospecting
title_fullStr Review of Processing and Interpretation of Self-Potential Anomalies: Transfer of Methodologies Developed in Magnetic Prospecting
title_full_unstemmed Review of Processing and Interpretation of Self-Potential Anomalies: Transfer of Methodologies Developed in Magnetic Prospecting
title_sort review of processing and interpretation of self-potential anomalies: transfer of methodologies developed in magnetic prospecting
publisher MDPI AG
series Geosciences
issn 2076-3263
publishDate 2021-04-01
description The self-potential (SP) method is one of the most inexpensive and unsophisticated geophysical methods. However, its application is limited due to the absence of a reliable interpreting methodology for the complex geological-environmental conditions. To exclude disturbances appearing in the SP method, a few ways for their removal (elimination) before quantitative analysis are presented. A brief review of the available interpretation methods is included. For the magnetic method of geophysical prospecting, special quantitative procedures applicable under complex physical-geological environments (oblique polarization, uneven terrain relief and unknown level of the normal field), have been developed. The detected common peculiarities between the magnetic and SP fields make it possible to apply the advanced procedures developed in magnetic prospecting to the SP method. Besides the reliable determination of the depth of anomalous targets, these methodologies enable the calculation of the corrections for non-horizontal SP observations and to determine the orientation of the polarization vector. For the classification of SP anomalies, is proposed to use a new parameter: the ‘self-potential moment’. The quantitative procedures (improved modifications of characteristic point, tangent techniques and the areal method) including the determination of the SP vector and SP moment, have been successfully tested on models and employed in real situations in mining, archaeological, environmental and technogenic geophysics. The obtained results indicate the effectiveness of the presented methodologies.
topic quantitative analysis
complex geological environments
self-potential moment
polarization vector
ore deposits
archaeological sites
url https://www.mdpi.com/2076-3263/11/5/194
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