摘要
金平—绿春金矿带空间上与中、酸性岩体分布关系密切。地面高精度磁测可圈定与金矿化有关的蚀变体范围,并推断隐伏斑岩体侵入状态。进而揭示磁异常与金矿化之间的关系,对深部金矿化远景进行评价。
This area is in the Jinping - Luchun Au metallogenetic zone and related close to the intermediate -acid rock body. The surface high precision magnetic survey can outline the area of alteration body related to the Au metallogenesis, infer the intrusion atate of buried porphyry body and show the relationship between magnetic anomaly and Au metallogenesis, thus assess the potentiality of Au metallogenesis in deep.
出处
《云南地质》
2013年第2期195-198,共4页
Yunnan Geology
关键词
金矿化体
近斑岩正磁异常
高精度磁测
远景评价
云南元阳岩甲
Au Metallogenetic Body
Positive Magnetic Anomaly near Porphyry Body
Potentiality Assessment
High Precision Magnetic Survey
Jinping-Luchun Au Metallogenesis Zone
