Technology of prospecting, exploration and forecasting of mineralisation areas of magmatic deposits

exploration and discovery of prospective

copper ore deposit.

A new method (method) of in-depth forecasting of magmatic copper deposits

A new method (method) for deep prediction of magmatic copper deposits, based on the isotopic

The result of the scientific and technical activity is a new method (method) of depth forecasting of magmatic copper deposits based on isotope studies and long-wave sounding

subsurface subsurface sounding. In the subsoil market

On the subsurface market there is a high demand for scientifically based

In the subsurface market there is a strong demand for scientifically based, predictive evaluation of small deposits and ore occurrences,

which prospects from the surface are uncertain. This

uncertainty often leads businessmen to

The uncertainty often leads businessmen to take unjustified risks of investing funds in

This uncertainty often leads businessmen to unjustified risks of investing funds in geological prospecting works on unpromising objects.

Existing prognostic estimates of ore objects

are based mainly on surface factors and

traditional geophysical methods.

The priority of surface factors is flawed in the sense that

All magmatic deposits are formed in the bowels and

sometimes deep from the present-day earth’s surface.

The surface factors always reflect the distorted in one way or another

to one degree or another the situation existing at depth.

Geophysical methods obtain a physical anomaly, but

Often without drilling exploration wells they are unable to determine what they are dealing with.

are able to determine what they are dealing with at depth,

such as graphitic shales or sulphide

ores. The methods developed and used in the

The methods developed and used in the technology proposed for commercialisation allow us to

objectively and accurately identify the substance causing the

situation and avoid the risks before the decision to proceed to

of the decision to proceed with exploration.

Khasen B. P.

Zeinullin A.A.

Lis S.N.

A.A. Kasimov

Baltabekova G.M.

Orynbek T.J.