CAJ | 학술논문

传统地球化学理论认为火山岩型铀矿的热液铀矿床中的铀都是通过氧化溶液搬运的，并由六价还原成四价而沉淀成矿；或者是是碱交代作用形成的。但大量的文献表明，铀的成矿不仅与火山岩和次火山岩有关，还与深源的中基性岩有关。
전통지구화학이론인위화산암형유광적열액유광상중적유도시통과양화용액반운적，병유륙개환원성사개이침정성광；혹자시시감교대작용형성적。단대량적문헌표명，유적성광불부여화산암화차화산암유관，환여심원적중기성암유관。
Conventional geochemical theory suggests that Volcanic hydrothermal uranium deposits of uranium are uranium oxide solution by handling, Price reduced by six tetravalent and ore deposits; or the formation of alkali metasomatism. But a lot of literature suggests that uranium mine raliza,tion not only with the volcanic and subvolcanic rocks, but also with deep source of the mafic rocks.