摘要
2012年在金寨银水寺地区开展了多金属矿调查评价,为了更加详细的了解银水寺向斜构造、佛子岭岩群底部钙质岩层的分布特征及其推覆构造面的产状,2013年采用CSAMT法对异常区进行了测量,结果表明CSAMT法在了解推覆面和寻找断层中有很好的反映。
Polymetallic ore survey and evaluation were carried out in the Yinshuisi area in Jinzhai in 2012. To better understand the Yinshuisi syncline structure, distribution features of calcareous rock bed at the bottom of the Foziling group complex and the occurrences of its nappe structure plane, CSAMT method was applied in surveying in the anomalous area and proved good in recognizing nappe plane and looking for faults.
出处
《安徽地质》
2016年第4期277-279,共3页
Geology of Anhui
