摘要
三架窝棚矿区位于桓仁盆地内的五里甸子隆起区,矿区主要出露界辽河群、青白口系,古生界寒武系、奥陶系和中生界白垩系地层。物性参数测量结果表明矿化体与围岩差异明显,具备较好的地球物理前提。通过物探测量在区内圈定6处异常高磁异常,4处极化率异常。通过初步分析认为。
The sangjiawopeng mining area is located in wulianzi uplift area in Huanren basin. the mining area mainly shows Liaohe group, qingbaikou system, Paleozoic CAMBRIAN, Ordovician and Mesozoic Cretaceous strata. The measurement results of physical parameters show that the mineralization body and surrounding rock are obviously different, which has a good geophysical premise. Six abnormal high magnetic anomalies and four polarization anomalies are delineated in the area by geophysical survey. Based on the preliminary analysis, f1 fault zone and C5 abnormal zone are the key points in the next step
作者
车晓光
CHE Xiao-guang(Liaoning nonferrous geological survey and research institute, Shenyang 110013,China)
出处
《世界有色金属》
2018年第3期156-158,共3页
World Nonferrous Metals
关键词
高磁异常
极化率异常
找矿意义
high magnetic anomaly
anomaly of polarizability
prospecting significance
