Ag-Cu-Fe-Zn-Cd-As-Sb Mobilization in the Upper Part of the Oselské Pásmo Lode—An Unknown Story in the Evolution of Kutná Hora Ore District, Czech Republic

Kutná Hora ore district, one of the largest historical silver deposits in Central Europe, consists of nine major lodes with Pb-Zn-Ag mineralization hosted by high-grade basement rocks of the Kutná Hora Crystalline Complex in central part of the Bohemian Massif. We conducted a detailed electron-microprobe study of a previously unknown ore mineralization from the uppermost level of the Muzejní důl mine, which is a medieval mine located within the Ag-richest Oselské pásmo Lode, in the southern part of the ore district. An unusual nature of this ore mineralization, which originated during three respective stages, was found. The early stage comprises the hypogene mineralization commonly occurring in the southern part of the district, composed of pyrite, arsenopyrite, Fe,Mn-enriched sphalerite, galena, and (keno)argentotetrahedrite-(Fe) hosted in quartz and siderite-rhodochrosite gangue. The second stage was characterized by the corrosion of early vein fill followed by the crystallization of a specific suite of ore minerals anomalously enriched in Ag, Cu, Zn, Cd, As, and Sb, including galena, Cd-enriched and Fe-poor sphalerite, greenockite, bornite, Ag,As,Sb,Mn-bearing chalcopyrite, silver, gold, stephanite, As,Cu-bearing pyrargyrite, Ag-Cu- and Sb-As-bearing polybasite-pearceite group minerals and a suite of tetrahedrite-group minerals, the latter showing wide variations in Ag-Cu, Sb-As, and Fe-Zn-Cd contents. The origin of the second-stage mineralization is interpreted in hydrothermal remobilization of ore metals and metaloids from the early ore mineralization, which was mediated by surficial fluids characterized by elevated redox potential. The third stage comprises acanthite and probably also Ag-Cu minerals (stromeyerite, jalpaite, and mckinstryite), Cu-S phases (covellite, spionkopite, geerite), and an Ag-Cu-Hg mineralization. This late mineralization was likely related to the pre-Cretaceous weathering of the apical part of the ore deposit and to the associated supergene enrichment of deeper parts of the ore zone by descending Ag,Cu-bearing waters.