摘要
1986年发现桐树庄银异常,经20余年反复查证,终于在2008年经钻探验证,在上古生界蔡家凹岩组取得地质找矿的重要进展,反映了找矿工作中实践—认识—发现、再实践—再认识—新发现的过程,这一进展和过程具有一定的借鉴意义。
The Tongshuzhuang anomaly was discovered in 1986. On the basis of more than 20 years'repeated inspection, important oreprospecting advances were made in Upper Paleozoic Caijia'ao Rock Group in 2008 through drilling verification. This success reflects the process of practice-recognition-discovery and re-practice-re-recognition-new discovery, and hence has some reference value.
出处
《物探与化探》
CAS
CSCD
北大核心
2009年第4期411-416,共6页
Geophysical and Geochemical Exploration
关键词
异常查证
分散异常
隐伏花岗斑岩
桐树庄
nomaly inspection
dispersed anomalies
concealed granite porphyry
Tongshuzhuang