Resumen de Estudio de inclusiones fluidas en la mineralización de Bario y Cobre del Alt. Bergueda (Barcelona)
The mineralitation consists of the filling of metric cavities with karst morphology in Devonian dolomite. The mineralization is situated closely under an erosive surface covered by a sequence of Buntsandstein. Most of the filling in the cavities was precipitated from high brine solutions at low temperature.
