摘要
从三频激电相对相位法原理出发，阐明相对相位异常空间特征，识别矿致异常的标志，并用已知地质剖面佐证。
On the basis of the principle of tri-frequency IP relative phase method,this paper expounds spatial characteristics of relative phase anomalies and points out indicators of anomalies related to mineralization,which are evidenced with known geological sections.
出处
《物探与化探》
CAS
CSCD
1999年第2期104-106,共3页
Geophysical and Geochemical Exploration
