Ore-magmatic systems of copper-molybdenum deposits.

Abstract

Ore deposition concludes a complex cycle of transport and evolution of materials throughout the crust where magmatic and hydrothermal associations are being formed. The crystallization of magma chambers influences the formation of ascending fluid and T rises. The development of the ore-magmatic system results from the interaction of subcrustal mafic magma and fluids separating from it. There are two types of fluid in Cu-Mo deposits; the systems include both intrusive bodies and surrounding rock, but the fluid systems evolve separately from them.-R.E.S.