Pikarenya D. The forming of hydrothermal-metasomatitic mineralization in fault zones

It is investigational position and structural position of hydrothermal-metasomatitic mineralization in the areas of deep faults. It is shown the field re-searches, that deep and more high-level faults are characterized by the presence of the natural impulsive electromagnetic fields, what arising up at their forming and accompany all stages of their development. The conducted experimental researches from the study of influence of the thermal and electromagnetic fields on the specimens of mountain rocks show that they assist appearance and development of hydrothermal-metasomatitic mineralization in deep faults. In particular, they stipulate additional mobilization and migration of solutions and matter from rocks, provide the acceleration of flowing of physical and chemical reactions, allow to reduce the temperatures of dissociation of matters and mineralogenesis. On the basis of experimental data and geology-genesis conformities to law of development of metasomatose on concrete geological objects the geology-genetic model of forming of hydrothermal-metasomatitic mineralization is in the areas of deep faults is formulated. It behaves to the group of hydrothermal-metamorphism models of ore-forming. In theory reasonable and the geology-geophysical searching criterion of areas of display of mineralization, which is related to the change to drawing magnetic and impulsive electromagnetic the fields, is practically confirmed.