摘要
缅甸中部德碑甄金矿受构造控制,根据矿物共生组合关系可分为金—黄铁矿—石英脉型与金-黄铁矿为主的多金属硫化物—方解石、石英脉型,矿石中金属硫化物含量高。投入激发极化法探测,选用合理的装置,可以准确地圈定矿化体的空间展布。
The Debeizhen gold deposit in central Burma is controlled by tectonic structure. It can be classified into gold-pyrite-quartz vein type and polymetallic sulfide - calcite and quartz vein type dominated by gold-pyrite according to mineral intergrowth association. The spacial distribution of mineralization can be precisely outlined by IP prospecting method with appropriate equipment as there are high content of metallic sulfides in the ores.
出处
《矿产与地质》
2004年第4期380-382,共3页
Mineral Resources and Geology
关键词
激发极化法
应用效果
金矿
缅甸曼德勒德碑甄矿
IP, application effect, gold deposit, the Debeizhen deposit, Mandalay, Burma
