Geology and mining - GPS Developer of Mineral Resources LTD

ERS (Remote Sensing of the Earth) methods are promising in identifying the patterns of distribution of minerals.

On the basis of a comprehensive interpretation of remote sensing data, criteria for the distribution of deposits of fuels (oil shale and others) and ore minerals (Copper, Zinc, Lead, Gold, Aluminum, Iron ore, Brown and Coal and others) can be established.
The relevance of the problem of forecasting and prospecting for minerals using remote sensing methods is due to the need to obtain qualitatively new data on the objects under study costs for costly field and overburden operations. Remote sensing covers large areas, including areas that are difficult to access by traditional methods.

The use of aerospace information in geology allows solving the following problems:

prediction of mineralization based on remote sensing data;
identification of natural anomalies, ore-controlling structures;
creation of landscape maps;
study of the structural forms of the lithosphere;
clarification, detailing of the geological structure.

Based on the remote sensing data, geotechnical maps are created at any convenient scale. These data are used in carrying out geological and mine surveying works.

The use of remote sensing in geology makes it possible to obtain fundamentally new information about the geological structure of an area, to quickly assess the structural features of objects, to select the most promising areas for setting up large-scale geological mapping, prospecting geophysical and drilling operations.

Core drilling

The essence of the method is used to perform geological exploration wells with great depth, drilling in rocky horizons, laying artesian wells. The method has a number of advantages, which are the mobility of installations, the possibility of sampling rocks. Extraction of core material to the surface allows us to study the geology of the site and justify the prospect of further research and development, to confirm the result of remote sensing of the earth with a result of 100%, by studying spectral analysis at the site of core samples, as well as the result from an independent laboratory.