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本文所讨论的锡矿床在一个大区域内(35km)展布,从捷克斯洛伐克的新姆埃斯托普斯尔克姆镇向西延伸到波兰乌伊切斯齐切镇以东。主岩为斯塔卡梅里卡山前寒武系变质片岩(厚约700—800m)。Wiszniewska(1982)将该片岩分为四种主要岩石类型:
The tin deposits discussed in this article are spread over a large area (35 km) extending westward from the town of New Mista Stkkarm in Czechoslovakia to the east of the town of Kozhiche, Poland. The main rock is the Precambrian metamorphic schist (about 700-800 m thick). Wiszniewska (1982) classified the rock into four main rock types: