Oil and Gas Exploration - The Gravimetric Approach Using Subsurface G-Anomalies
Abstract
Earth’s diverse topography—including mountains, valleys, underground caverns, oceans, and glaciers—results in variations in surface mass. Since gravity is directly related to mass, slight variations in the gravitational field exist across the planet’s surface. The gravimetric method is a non-destructive geophysical technique used to measure these differences in Earth’s gravitational field at specific locations. Although the changes in gravity may be subtle, they provide critical clues to understanding the structure and composition of the solid Earth and other related phenomena. The observed surface gravity, g, results from the attraction of mass within the Earth’s interior. This work aims to highlight the practical importance of the gravimetric approach in detecting subsurface anomalies, especially in oil and gas exploration. The most commonly used data are Bouguer gravity anomalies, which reflect variations in the gravitational field caused by objects of interest, such as hydrocarbon deposits. These variations can be analyzed using various analytical and computational methods to estimate the depth, geometry, and density of the causative bodies. Therefore, this study reveals that gravimetric methods have wide applications in geophysics, engineering, environmental science, and geosciences.
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