摘要
Recently, the Xin Jie layered intrusive body has been recognized in the Trap Province of SW China, which can be divided into three igneous cumulate cycles. It shows considerable similarities with the Hong Ge titanmagnetitebearing layered intrusive body in petrography and mineralization although the ore beddings near the footwall are much higher in the grade of chromium and platinum. It is suggested that the Lu Ku Intrusive Crowd, to which the Hong Ge and Xin Jie intrusives belong, in the Trap Province of SW China is probably formed in;such an environment as Palaeozoic An Ning River rift.
Recently, the Xin Jie layered intrusive body has been recognized in the Trap Pro-vince of SW China, which can be divided into three igneous cumulate cycles. It shows considerable similarities with the Hong Ge titanmagnetitebearing layered intrusive body in petrography and mineralization although the ore beddings near the footwall are much higher in the grade of chromium, and platinum.It is suggested that the Lu Ku Intrusive Crowd, to which the Hong Ge and Xin Jie intrusives belong, in the Trap Province of SW China is probably formed in such an en-vironment as Palaeozoic An Ning River rift.
出处
《地球化学》
CAS
1981年第1期66-73,i004,共9页
Geochimica
