CAJ | 학술논문

云南东部宣威-罗平一带，在二叠纪玄武岩两大喷发旋回顶部的古风化壳中，发现两层稀土、铁、钛多金属矿化层：ΣREO 0.016%~0.52%、TFe 10.09%~49.44%、TiO21.08%~10.94%；含矿层厚度8.0~35.0 m；矿化体分布广，呈层状、似层状。矿化层的形成经历了源(富稀土、铁、钛的玄武岩)-转(古风化淋积作用)-储(有利古地理环境)的成矿机理，成为稀土、铁、钛多金属矿极具潜力的远景区。
운남동부선위-라평일대，재이첩기현무암량대분발선회정부적고풍화각중，발현량층희토、철、태다금속광화층：ΣREO 0.016%~0.52%、TFe 10.09%~49.44%、TiO21.08%~10.94%；함광층후도8.0~35.0 m；광화체분포엄，정층상、사층상。광화층적형성경력료원(부희토、철、태적현무암)-전(고풍화림적작용)-저(유리고지리배경)적성광궤리，성위희토、철、태다금속광겁구잠력적원경구。
In Xuanwei-Luoping area of eastern Yunnan Province, two REE, Fe, Ti polymetallic mineralized beds were discovered at the tops of paleoweathering crusts formed by two eruptive cycles of Permian basalts. The thickness of the ore-bearing beds is 8.0~35.0 m, and they containΣREO 0.016%~0.52%, TFe 10.09%~49.44%and TiO2 1.08%~10.94%. Mineralized bodies are widely distributed and assume stratified and stratoid forms. The formation of the mineralized bed experienced the metallogenic mechanism of initial source formation (basalts rich in REE, Fe and Ti) -transformation (leaching and infiltration of paleoweathering crust) -storage (stored in favorable paleogeographic environment), and hence this area has become a prospective area of great potential for REE, Fe, Ti polymetallic deposits.