Geochemical modelling of ore-forming processes in the Börzsöny Mountains, N-Hungary
This study utilizes PHREEQC 3.0 geochemical modeling to demonstrate that the reduced porphyry mineralization in the central Börzsöny Mountains resulted from multiple fluid pulses characterized by fluctuating temperature, redox conditions, and sulfur fugacity, which successfully constrained the observed paragenetic sequence of sulfide precipitation and alteration.