Geochemical exploration aims to locate areas with anomalous concentrations of elements or compounds associated with mineral deposits, thereby assisting in the discovery of new mineral resources.

Copper mineralization is often associated with the presence of copper-bearing minerals, such as chalcopyrite (CuFeS2) and malachite (Cu2CO3(OH)2).

Geochemical analysis involves the determination of the chemical composition of rocks, minerals, and fluids using various analytical techniques, such as atomic absorption spectrometry, inductively coupled plasma mass spectrometry, and X-ray fluorescence spectrometry.

A local anomaly is a geochemical anomaly that is confined to a specific area and is often associated with the presence of a mineral deposit.

Pathfinder elements are chemical elements or compounds that are associated with a particular mineral deposit and can be used to trace the location of the deposit.

Soil gas analysis involves the collection and analysis of gases released from rocks and soils to detect anomalies in the concentrations of certain gases, such as hydrocarbons and carbon dioxide, which may be associated with mineral deposits.

Stream sediment sampling involves the collection and analysis of fine-grained sediments deposited in stream channels to identify anomalous concentrations of elements or compounds that may have been transported from upstream mineral deposits.

Heavy mineral analysis involves the separation and identification of heavy minerals, such as magnetite, ilmenite, and zircon, in stream sediments or soils to identify areas with potential mineral deposits.

Hydrogeochemical analysis involves the determination of the chemical composition of water samples, including groundwater, surface water, and spring water, to identify anomalies in the concentrations of elements or compounds that may be associated with mineral deposits.

Biogeochemical analysis involves the analysis of vegetation, such as leaves, twigs, and roots, to identify anomalous concentrations of elements or compounds that may have been absorbed from the soil or groundwater, indicating the presence of mineral deposits.

Lithogeochemical analysis involves the determination of the chemical composition of rock samples to identify anomalous concentrations of elements or compounds that may be associated with mineral deposits.

Geochemical soil sampling involves the collection and analysis of soil samples to identify anomalous concentrations of elements or compounds that may have been transported from nearby mineral deposits or may be indicative of the presence of mineral deposits.

Fluid inclusion analysis involves the study of fluid inclusions, which are small pockets of fluid trapped within minerals, to obtain information about the chemical composition and temperature of the fluids that were present during the formation of the minerals.

Isotope analysis involves the determination of the isotopic composition of elements in rocks, minerals, and fluids to identify anomalies in the ratios of different isotopes, which can provide information about the age, origin, and processes involved in the formation of mineral deposits.

Geochemical interpretation involves the integration and analysis of geochemical data, including the identification of geochemical anomalies, pathfinder elements, and geochemical trends, to identify areas with potential mineral deposits.