Fe-sulfates from magnesite deposit Bankov near Košice (Slovakia)
Geoscience Research Reports 38, 2005 (GRR for 2004),
pages 110–110
Abstract
In the abandoned mine of magnesite deposit Bankov near Košice an interesting association of Fe-sulfates occur, which originated after oxidation of marcasite. Fe-sulfates are represented mainly by brown 0,5-2 mm sized crystals and light rose powder aggregates of romerite. Yellow aggregates of copiapite and light green aggregates of melanterite occur together with romerite.