Fluid inclusion and stable isotope study of the Kasejovice gold district, central Bohemia

Abstrakt

Quartz gangue from the Variscan gold-bearing Kasejovice district (Jakub Mine) of the Moldanubian Drosendorf Unit, Bohemian Massif, was studied by fluid inclusion, stable isotope and SEM-CL techniques.

Klíčová slova

• gold
• hydrothermal processes
• fluid inclusions
• oxygen isotopes