ИСТИНА

Geology studies various rocks. The study of petrography is based on magmatic rocks that are formed from hot magmatic melts. When the magma is cooled to a solid phase, various minerals pass successively. In the last place, as a rule, they are compounds of platinum, iron, etc. At what the content and distribution of them in the host rock is not uniform. The purpose of this work is to establish mechanisms and conditions for the formation of sulfide mineralization in intrusive layered massifs. The effectiveness of mass transfer and accumulation of sulphides during solidification of hot magmatic melt of intrusions depends to a large extent on the possibility of wetting of the rock-forming silicate grains and the porosity of the host environment by the sulphide liquid. These relationships are deciphered by the morphology of the sulfide phases and their distribution over the volume of the rocks. Obtain this information by modern methods of computer X-ray tomography.