摘要
由于岩矿体剩余磁化强度与感应磁化强度的差异导致岩矿磁异常差异及磁偏角、磁倾角的不同，根据这一特征来判别异常性质。
Rock and ore body are different in their remanent magnetization and induced magnetization leading to different anomaly and different magnetic declination and magnetic inclination Therefore the difference can be used to judge the anomaly natures.
出处
《地质找矿论丛》
CAS
CSCD
1995年第3期70-79,共10页
Contributions to Geology and Mineral Resources Research
