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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书目信息
出版者
La Societe Geographique de Liege
其它主题
Disolucion; Elementos metalicos; Capa freatica; Element metallique; Genesis del suelo
语言
英语
注释
Summaries (En, Fr)
3 ill.; 6 ref.
ISBN
2-87298-004-0
类型
Conference; Summary
来源
Proceedings of the European conference on speleology. Physical speleology and karstology, Grimberieux, J.Ek, C. (eds).- Liege (Belgium): La Societe Geographique de Liege, 1993.- ISBN 2-87298-004-0. p. 87-92
粮农组织大会
Conference Europeenne de Speleologie : Speleologie Physique et Karstologie, Helecine (Belgium), Aug 1992
1995-08-15
AGRIS AP