Reconstruction of hydrothermal karst system in Zn-Pb sulphide deposits (Upper Silesian region, Poland)
1993
Sass-Gustkiewicz, M. (Mining and Metallurgy Univ., Krakow (Poland). Inst. of Geology and Mineral Deposit)
In the Upper Silesian district the ore bodies form vertically developed structures at lower levels of the deposits upwards grading into horizontally disposed structures. Both are interpreted as belonging to the same endogenic, hydrothermal kars system produced by ascending mineralized solutions. All the evidences point out to close genetic relationships between the dissolution of host rocks an the deposition of ores in the evolving karst system.
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