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苏台德地区发现铀矿化的远景是与地台发育期的沉积层有关的,沉积物是在华力西期内生金属矿成矿过程结束后堆积而成的。主要远景典型为苏台德中部的砂岩型矿床(石炭纪上部、中石炭—泥盆纪的陆相沉积和部分斯蒂芬统)。苏台德西部同一个年代的(北苏台德向斜)岩性相似的岩层也属于
The prospect of uranium mineralization in the Su-Teide region was related to the sedimentary layers of the platform during the deposition. The sediments were deposited after the endogenous metallogenic ore-forming process in the Haryclinal period ended. The main prospect is typically sandstone-type deposits in central Sudeten (Upper Carboniferous, Middle Carboniferous-Devonian terrestrial deposits and part of Stephen’s System). Similar rock formations of the same origin (in the northern Sudedean syncline) in the western Sudete belonged to this area