
Авторы:
Дата издания
17.05.2023На каком языке издана
ISSN
17282713Тип исследования
Аннотация (краткое описание)
The purpose of the studies presented in the article is to obtain the information of the deep structures along the Shu-Sarysu geotrav-erse, to determine the regularities in the distribution of mineral deposits and predictive assessment of the research area prospects for searching for hydrocarbons and other minerals. To achieve this purpose, a complex of high-precision gravitational and magnetometric measurements was used. There was shown a high efficiency of the integrated interpretation of 3D gravimagnetic modeling when studying the geological structure of the crystalline basement (assessment of the morphology of its surface, material-petrophysical mapping of the rocks that make up the basement) and the sedimentary cover (assessment of the morphology of the reference horizons, studying their material composition); when identifying and clarifying the position of discontinuous faults, conducting lineament analysis in order to decipher the block structure of the studied areas; when building 3D volumetric models of geophysical parameters; when substantiating predictive and search geophysical criteria for detecting oil and gas geological structures, both in the thickness of sedimentary formations and in the rocks of the crystalline basement. The progress of these methods is conditioned by the widespread introduction into practice of modern computer technologies for processing and interpreting dataDOI
10.17721/1728-2713.102.05Практическое значение
The results of the study can be applied to improve geological exploration and resource assessment in the Shu-Sarysu sedimentary basin. The developed 3D gravity-magnetic models enhance the identification of deep geological structures, fault systems, and prospective hydrocarbon and mineral-bearing zones, thereby increasing exploration efficiency, reducing geological risks, and supporting more informed decision-making in exploration programs.Impact Factor
0.8Количество цитирований
3Данный документ располагается в коллекциях
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Вісник_Геологія_№102_5.pdf