Abstract
The Herja ore deposit is one of the most known of the Baia Mare Neogene metallogenetic district and is associated with a complex stock of Pannonian age. The hydrothermal alterations associated with the mineralizations are represented by: the propylitization, the argillization, the phyllic and potassic alteration. The monoascenedant character of the mineralizations is predominant. The magmatic intrusions have been sequential placed and have represented the heat, metals and hydrothermal solutions source. In the first stages of mineralization the hydrothermal solutions contain predominantly magmatic water and in the final stages the water is of connate and meteoric origin. According to the structural magmatic control, to the mineralogical composition and to the hydrothermal alterations, the Herja ore deposits are of a low sulphidation epithermal systems type.
Recommended Citation
Damian, Gheorghe
(2003)
The genesis of the base metal ore deposit from Herja,
Studia UBB Geologia
48
(1): 85-100
DOI: http://dx.doi.org/10.5038/1937-8602.48.1.8
Available at:
https://digitalcommons.usf.edu/geologia/vol48/iss1/art8
