摘要
冀东孤山子航磁异常为冀东三大航磁异常之一,且位于冀东石人沟-板城铁矿集中区。通过对本区地质构造特征、岩矿石物性及重磁异常特征等进行综合研究,认为孤山子航磁异常并非完全由孤山子基性-超基性岩杂岩体和已控制的浅地表超贫磁铁矿体所引起,进而采用2.5D拟合技术进行了定量拟合计算和资源量估算,认为孤山子航磁异常具有较好的找铁矿前景。同时,通过对孤山子航磁异常的推断解释,总结了减少航磁异常解释多解性的思路与做法。
The aeromagnetic anomaly in the Gushanzi area is one of the three major aeromagnetic anomalies in eastern Hebei Province,which is located in the Shirengou-Bancheng iron ore concentration area.Studies of its geological structure,physical properties of rocks and ores,as well as its gravitational and aeromagnetic anomalies suggest that the Gushanzi mafic-ultrabasic intrusive complex and shallow ultra-low-grade magnetite ore are not completely responsible for this aeromagnetic anomaly.The results of 2.5D quantitative calculation and resource estimation indicate that the Gushanzi aeromagnetic anomaly may imply a promising potential for iron ore.And through interpretation of the Gushanzi aeromagnetic anomaly,this paper summarizes the ideas and methods of reducing ambiguity in interpretation of aeromagnetic anomalies.
出处
《地质与勘探》
CAS
CSCD
北大核心
2012年第4期750-759,共10页
Geology and Exploration
基金
地质大调查项目"重要铁矿成矿区带航磁靶区优选"(项目编号为1212010913037)
关键词
航磁异常
铁矿
超贫磁铁矿
找矿前景
aeromagnetic anomaly; iron ore; ultra-low-grade magnetite; prospecting potential