摘要
描述宁芜地区铁磷矿床的成矿机理。探讨了岩浆及热液铁、磷、钛、稀土等的搬运形式及成矿过程。结果表明，氢化物是成矿物质的主要迁移形式，它们迁移至地壳浅部被氧化成矿。
The paper describes the formation mechanism of iron and phosphorous ore deposits in the Ningwu area and discusses on the migration mode and metallogenic process of magmatic and hydrothermal iron,phosphorous,titanium,REE,etc.. It is indicated that hydrogen compd. is the major form in which metallogenic substance migrated to the shallow crust and mineralized by oxidation.
出处
《安徽地质》
2000年第4期265-271,282,共8页
Geology of Anhui
关键词
铁磷矿床
氢化物
搬运形式
成矿机理
宁芜地区
iron and phosphorous ore deposit
hydrogen compd.
migration mode
metallogenic mechanism
Ningwu area
