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波兰的自然硫矿床产在喀尔巴阡前缘拗陷的中新世海相沉积岩层中。该岩层可划分为三个岩相:氯化物岩相,分布在喀尔巴阡山的边缘带;硫酸盐岩相,占据前缘拗陷的大部分;碳酸盐岩相,分布在前缘拗陷的边缘带内。一些老的硫矿床及矿点主要集中在克拉科夫与布斯克之间的硫酸盐岩相的边缘带内。自第二次世界大战结束之后,在喀尔巴阡前缘拗陷进行更为详细的硫矿普查,根据对中新世岩层研究的结果,于1952年在塔尔诺布热克地区发现了一个大而隐伏的自然硫矿床。喀尔巴阡前缘拗陷的中新世海相岩层是一个年青的构造层,在波兰出露一部份,向东延伸到苏联乌克兰、罗马尼亚、保加利亚,向西进入捷克斯洛伐克和奥地利境内(图1)。
Natural sulfur deposits in Poland are produced in Miocene marine sedimentary formations in the Carpathian frontier depression. The rock can be divided into three lithofacies: chloride facies, distributed in the Carpathian marginal zone; sulfate facies, accounting for most of the leading edge depression; carbonate facies, distributed in the leading edge of the bend The edge of the trap band. Some of the old sulfur deposits and ore deposits are mainly concentrated in the marginal zone of the sulfate phase between Krakow and Busqui. Since the end of World War II, a more detailed sulphurous census has been conducted in the Carpathian frontier depression. Based on the results of the study on the Miocene strata, it was discovered in Tarnobregek in 1952 A large, hidden natural sulfur deposit. The Miocene marine rock formation in the Carpathian frontier depression is a young tectonic layer that is partially exposed in Poland and extends eastward to the Soviet Union of Ukraine, Romania, Bulgaria and westward into Czechoslovakia and Austria ( figure 1).