摘要
介绍了应用系统核和核度理论对化探异常进行评判的过程，初步试验证明。
The geochemical anomalies are divided into the one related to mineralization and the other not related to mineralization. The origin of anomalies related to mineralization is orebodies. Orebody and its anomaly consist of anomaly system. The core of anomaly system is the orebody, and the system does not exist without the core. The method for evaluating geochemical anomalies by aid of the theory of core of system is introduced, which was proved to be effective by practice.
出处
《地质与勘探》
CAS
CSCD
北大核心
1998年第6期40-43,共4页
Geology and Exploration
基金
浙江省自然科学基金
