Genetic aspects of the Recsk mineralized complex, Hungary.

Abstract

Mineralization in this area belongs to the Palaeogene volcanic arc. The main phases, culminating in porphyry copper, result from hydrothermal events related to a diorite porphyry intrusion. Late-stage mineralization is thought to be a product of remobilization. It appears that the Recsk deposit has an affinity with island-arc type magmatism. -R.E.S.