摘要
氟镁石(MgF_2)是一种罕见矿物,四川省偏岩子金矿床为氟镁石—石英—多金属硫化物—自然金矿石结构的罕见类型矿床。研究其成因和成岩成矿机制,对于地球化学、矿物学、矿床学包括此后的矿产开发非常有意义。
Magnesium fluoride, including MgF_2, is a rare mineral. The Pianyanzi gold deposit in Sichuan is a deposit of rare style, which is concluded by magnesium fluoride, quartz, polymetallic sulfide and natural gold ore. So it's very significant for mineral development to study the genesis and diagenetic mineralization mechanism of the deposit.
出处
《世界有色金属》
2016年第3S期116-117,共2页
World Nonferrous Metals
关键词
氟镁石
包裹体
氢化物
magnesium fluoride
inclusion
hydride