Geophysical research: article

THE GRAVITY FIELD POWER SPECTRUM AND THE DEEP STRUCTURE OF THE AJINOUR REGION (AZERBAIJAN)
A.H. Kadirov A.H. Zamanova G.R. Sadigova Kh.G. Mustafayeva
Geology and Geophysics Institute, Ministry of Science and Education of the Azerbaijan Republic
Journal: Geophysical research
Tome: 25
Number: 1
Year: 2024
Pages: 57-68
UDK: 550.831.015.072
DOI: 10.21455/gr2024.1-4
Full text
Keywords: power spectrum, Spector-Grant method, Hartley transformation, Butterworth filter, gravity anomaly, Ajinour region
Аnnotation: The results of the study of gravity anomalies using numerical methods and the deep structure of the Ajinour re-gion with expected oil and gas potential are presented. The analysis of gravitational field anomalies was carried out using the Hartley transformation and the Butterworth filter. The deep position of the masses creating the anomaly was calculated using the Spector–Grant method based on the values of the gravitational field power spectrum. The results of studying the power spectrum of the gravitational field made it possible to determine the frequency (wave number) of the cutoff and the average depth of the sources of gravitational anomalies. It was revealed that the geodensity boundaries that create gravitational anomalies in the studied region are located at the depths of 5 and 18.5 km. The regional and local components were identified using high-frequency and low-frequency filtering of gravitational field and compared with the results of geophysical seismic observations. It was assumed that the boundary forming local anomalies is located on average at the depth of 5 km and is associated with the surface relief of Mesozoic deposits. This is independently confirmed, since according to seismic exploration and drilling data in the Ajinour region, Mesozoic deposits occur at a depth of 5–6 km. An analysis of the gravity anomalies in the study area reveals that there are no pronounced anomalies such as the Ismayilli maximum and the Middle Goychay protrusion throughout the Alazan-Ayrichay minimum zone. Although there are morphological signs of quite numerous weaker anomalies, manifested as distortions in the isolines on the gravity map.
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