Mineral exploration is the process of finding commercially viable concentrations of minerals to mine. It involves a range of activities aimed at discovering new mineral deposits, evaluating the potential of existing deposits, and determining the feasibility of mining these resources.
Geological exploration for mineral resources (Geological mapping) using Remote Sensing (RS) methods - non-traditional exploration for indirect presence of mineral resources based on satellite, aerial, and UAV sensors in a wide electromagnetic spectrum.
Images are collected either through optical sensors or radar sensors with synthetic aperture. Optical sensors measure spectral data of sunlight reflected from the Earth's surface. Synthetic aperture radar (SAR) sensors can detect electromagnetic data by transmitting microwave radiation and receiving backscattered waves from the Earth's surface.
Remote sensing images are used for indirect exploration of valuable mineral deposits in two key ways:- Mapping and analyzing the geology, faults, and fractures of the ore deposit.
- Identification of hydrothermally altered rocks based on their spectral characteristics.
Mapping hydrothermal alteration minerals and structural lines, for example, using multi-spectral images from satellites like Landsat 8 (or Aster), provides valuable information for mineral exploration. For instance, gold mineralization occurs as quartz veins and stringers associated with hydrothermal alteration halos. Faults are interpreted as pathways for mineralizing fluids, where the interaction between host rocks and hydrothermal fluids causes variations in composition. Detecting these features using RS methods is a key indicator for targeting new prospective areas of orogenic gold mineralization. For example, remote sensing image processing methods such as band combinations, band ratios, and principal component analysis (PCA) have been applied to visible, near-infrared, and short-wave infrared ranges from Landsat 8 satellite.