IMPROVED METHODОLOGY OF DETAILED MAGNETOMETRIC SURVEY TO SOLVE THE PROBLEMS OF OIL AND GAS GEOLOGY-Reference-Cited by-同舟云学术

IMPROVED METHODОLOGY OF DETAILED MAGNETOMETRIC SURVEY TO SOLVE THE PROBLEMS OF OIL AND GAS GEOLOGY

Published:2024 Issue:2 (105) Volume: Page:29-36
ISSN:1728-2713
Container-title:Visnyk of Taras Shevchenko National University of Kyiv. Geology
language:
Short-container-title:VKNUGEOL

Author:

,VYZHVA Serhii^ORCID,POPOV Serhii^ORCID, ,BONDAR Kseniia^ORCID, ,HOMENKO Ruslan, ,IVKO Аnton, ,ANDRIICHUK Yuliia, ,KRUHLOV Bohdan^ORCID, ,KRUGLOV Оlersandr^ORCID, ,POLYACHENKO Ievgen^ORCID,

Abstract

Background. Nowadays, interest in studying the local anomalous magnetic field to solve the problems of oil and gas geology is growing, and the capabilities of the equipment can significantly increase the speed, accuracy and detail of work. Accordingly, the development and testing of an improved method of detailed magnetic recording in motion becomes relevant. Methods. For areas with low gradient magnetic field, we assessed the accuracy of the survey by comparing the maps obtained from repeated surveys of the site. Results. The survey of the magnetic field was conducted in the movement. The total surveyed area was about 20 square kilometers in the Zinkovsky district of the Poltava region. The inter-profile distance was about 50 meters, the distance between the points of observation on the profile was about 1 meter. This grid of observations allows us to get maps that differ significantly from the maps obtained by the usual density of observations. This technique also allows identifying local anomalies, and drawing conclusions about the fine structure of the magnetic field. The main objects that form anomalies and their geological characteristics are identified. On this basis, interpreted magnetic field anomalies in oil and gas regions were catalogued. Conclusions. We have proposed explanation of tectonic and geochemical factors, which form local anomalies of the magnetic field of the studied areas. Three types of anomalies associated with ravines are distinguished. Positive anomalies over ravines and step-type anomalies, in our opinion, are associated with tectonic movements, and negative anomalies are due to slope wash processes. Alternating magnetic fields in the studied areas may be due to ferruginized deposits.

Publisher

Taras Shevchenko National University of Kyiv

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