Mineral Characterization, Hydrothermal Alterations, Oxides, and Clays

At APEX, we provide detailed analysis for mineral characterization, allowing us to identify the composition, structure, and properties of minerals in geological samples.

This characterization is essential for understanding mineral deposits and optimizing extraction methods.

Hydrothermal Alterations: We study the effects of hot aqueous solutions on minerals. These processes can lead to the formation of secondary minerals and are key indicators in mineral exploration. Common alterations include silicification, carbonatization, chloritization, and the formation of oxides and clays.

Oxides and Clays: Oxides result from the oxidation of metals and are crucial for identifying alteration and weathering processes. Typical examples include hematite and limonite. Clays, on the other hand, are products of the decomposition of primary minerals and are vital in soil studies and alteration mapping. Common clays include kaolinite and montmorillonite.

To enhance characterization, APEX integrates remote sensing technologies such as ASTER sensors and WorldView-3 satellites. These advanced tools provide high-resolution imagery and thermal data that enable us to better characterize alterations and zone areas with higher acidity and temperature. By analyzing thermal signatures, we can precisely identify the locations where hydrothermal processes have occurred and pinpoint areas where clays and other minerals have formed due to alteration.

Our use of remote sensing data provides an additional layer of insight, allowing for more accurate mapping and zonation of alteration areas, optimizing exploration efforts and improving the understanding of mineral formation processes. This integrated approach ensures that our clients receive high-quality, actionable data for better decision-making and resource management.