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根据对沥青铀矿与方解石共生的矿床所查明的规律,作出了关于这些矿床形成条件的结论。第一次确定了各种硫化物被含铀的碳酸盐溶液所重新沉淀,因而在铀矿床中含铀细脉成分与围岩成分的关系表现很明显。描述了硫化物再沉淀时所伴随的现象及组成碳酸盐-沥青铀矿脉的各种矿物之间关系。
Based on the laws identified by the coexisting deposits of uraninite with calcite, conclusions have been drawn about the formation conditions of these deposits. For the first time, it has been determined that various sulfides are reprecipitated by uranium-bearing carbonate solutions and thus the relationship between uranium vein-forming elements and the composition of the surrounding rock is evident in the uranium deposit. Describes the phenomena associated with sulfide reprecipitation and the relationship between the various minerals that make up the carbonate-bitumen uranium veins.