Remote sensing methods help complement traditional geological prospecting work in oil and gas exploration by:
- identifying zones of anomalous hydrocarbon seepage;
- detecting increased thermal flow caused by active fluid-thermodynamic processes in reservoirs;
- assessing the dynamic state of the reservoir and the impact of contemporary tectonic movements on it.
Space imagery and visual observation allow the evaluation of the structural features of shelves, identifying large-scale geological structures that may contain (hydrocarbon) gas and oil deposits.
Studying geological structures in basins, especially lineament anomalies, through remote sensing methods, enables us to find a more precise and reliable approach to discovering hydrocarbon deposits formed under the influence of underground geological pressure and plate tectonics.
The full set of channels provided, for example, by Landsat 8 - 9 (OLI), is the most effective basic data used for studying lineaments, with a focus on visible channels and the panchromatic channel due to their spatial accuracy (when combined, for instance, with high-resolution satellite imagery).
Statistical analysis of lineaments is carried out to understand points of surface pressure and the orientation of geological structures present in the basin.
Lineament maps, lineament density maps, and lineament orientation maps are created to visually comprehend the topography layout. Surface temperature profiles, vegetation trends through NDVI, development of drainage networks, and soil surface profiles serve as indicators for delineating hotspots for oil and gas exploration.
Digital Elevation Model (DEM), thermal range, infrared range, and visible range from Landsat 8 - 9 (OLI) provide essential results for hydrocarbon prospecting.