Tectonic-magmatic processes accompaining the mineralization of phosphorus-uranium metasomatic formation

Uranium-zirconium-thorium-rare earth-phosphor mineralization was formed within intersection nodes of different-oriented folded systems within zones of intrafolded disruptive faults after introduction of granitoid intrusions and limbs, saddle-shaped bodies in hinges, tubeshaped and complex in form in blocking folds represent typical ones. Unlike phosphorus-uranium ones properly uranium and uranium-molybdenum deposits in the same regions are regulated by connection nodes of after-folded disjunctive faults, have different ore composition, different ore body morphology and thick zones of before-ore alterations by albilization type or hydronicaceous alterations when there is no connection with granitoid magmatism