摘要
钛磁铁矿产于角闪辉石岩、斜长角闪岩、角闪岩等变基性-超基性杂岩体中,是在深部构造活动控制和后期变质作用下形成的晚期结晶分异型矿床。
The titanomagnetite is formed in the metabasite and meta- uhrabasics complex of hornblende pyroxenolite, plagioclase amphibololite and amphibololite. It is an ore deposit of late crystal differentiation type formed under the control of deep structual activity and the late metamorphism.
出处
《云南地质》
2007年第1期124-128,共5页
Yunnan Geology
