摘要
钟姑地区位于长江中下游成矿带,具有优越的成矿地质条件。本文通过在测区开展面积性和剖面重磁电测量,以岩石物性为基础,用已有地质钻孔资料做约束,对物探数据进行处理和反演计算,推断13条控制性剖面-2000m以浅地质结构,结合界面反演等处理方法,获得了测区主要地层界面埋深数据,编制了各个深度的地质中断图;在此基础上进行典型矿区分析和总结,建立地质-物探成矿模式,在合理的定向分析及定量计算条件下,圈定找矿靶区。
Located in metallogenic zone along the mid-lower Yangtze River reaches, the Zhonggu area is superior in ore-forming geological conditions. This paper, through area and profile survey of gravity, magnetism and electricity in the mapped area, with physical properties of rocks as basis, and known geological borehole data as constraint, processed geophysical data, made an inversion calculation, inferred a geological structure above -2000m level within 13 controlling profiles, combined with interface inversion, acquired burial depth data of major stratigraphic interfaces in the mapped area, prepared geological interruption map of each depth, on such basis, analyzed and summarized typical ore districts, built up geological-geophysical ore-forming model, and outlined mineral exploration targets under reasonable orientation analysis and quantitative calculation.
出处
《安徽地质》
2016年第1期10-16,共7页
Geology of Anhui
基金
安徽省公益性地质(科技)工作项目(2009-07)资助
关键词
钟姑地区
重磁电
地质填图
找矿靶区
gravity,magnetism and electricity
geological mapping
mineral exploration targets
Zhonggu area