Abstract
Kasperske Hory, one of the largest gold deposits in the Bohemian Massif, is characterised by shear zone-related gold-bearing quartz veins at the tectonic boundary of the two metamorphic terranes of the Moldanubian Unit. Studies of the geology, mineral paragenesis, fluid inclusions and oxygen geothermometry have been carried out to determine the mineralisation events and alternative P-T-t model of this deposit.
The pre-mineralisation stage is characterised by geochemical evidence of pegmatites (similar to 700 C and 1.1-0.45 GPa) and metamorphic structures resulting from deformation Dx+1 at the regional metamorphic peak (650 degrees C and 0.5 GPa). The mineralisation in Dx+2 began to develop from the formation of the Q(1) and Q(2) quartz veins (Stage I) under brittle-ductile conditions with the N-S extension; these quartz veins were filled mainly by apatite, plagioclase-1, muscovite and arsenopyrite-1.
Revised and reinterpreted gechronological data indicate that the earliest quartz veins can be dated at 344 Ma. The Q(3) veins were formed later under brittle to brittle-ductile conditions with crystallisation of plagioclase-2, arsenopyrite-2, scheelite, chlorite, pyrite and calcite (Stage II).
The corresponding fluids of Stages land II belong to the C-H-O-N system. The P-T conditions correspond to 590-520 degrees C and to 0.44-0.25 GPa for Stage I and 480-390 degrees C and similar to 0.2 GPa for Stage II.
Stage III is characterised by the precipitation of younger quartz, chlorite, molybdenite, calcite, pyrrhotite-1, galena-1, native gold, bismuth, and other Bi-Te minerals; the associated aqueous fluids (salinity 1.5, 8 wt.% NaCI equiv.) follow fluid inclusion trails and were trapped at relatively low pressures and temperatures (290-180 degrees C and <0.1 GPa). Stage IV is mainly dominated by carbonate and fluorite fillings of the open fractures and cracks.
Arsenopyrite-1 and -2 and molybdenite are the main gold-bearing and gold-carrying ore phases at this deposit.