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根据磁异常特征预测红格岩盆底部大型铁矿 被引量:7

THE PREDICTION OF A LARGE-SIZE IRON DEPOSIT AT THE BOTTOM OF HONGGE LOPOLITH BASED ON MAGENTIC ANOMALY CHARACTERISTICS
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摘要 为了满足国家经济建设对矿产资源的需求量,我国加大了对深部矿山的勘查。笔者通过分析四川省攀枝花市红格地区的地质环境和成矿条件,以及对航磁异常、地面高精度磁测和地质钻探工作的研究,根据磁异常特征准确预测了红格岩盆存在大型的钒钛磁铁矿,阐述了该说明磁异常特征是预测岩盆底部大型铁矿一种找矿模式,是解决深部铁矿勘查最为有效的一种方法。 In order to meet the demand of mineral resources in national economic construction,China has strengthened the deep mine investigation.Based on an analysis of the geological environment and ore-forming conditions of Hengge area in Panzhihua with the emphasis placed on aeromagnetic anomaly,ground high-pecision magnetic survey and drilling work,the authors accurately predicted the existence of a large-ize vanadium titanomagnetite deposit according to magnetic anomaly characteristics.It is thus held that magnetic anomaly characteristics constitute an ore-rospecting model for predicting large-size ore deposits,and also serve as a most effective means for deep iron deposit exploration.
出处 《物探与化探》 CAS CSCD 北大核心 2010年第6期795-799,805,共6页 Geophysical and Geochemical Exploration
关键词 磁异常 岩盆 构造 找矿模式 攀枝花钒钛磁铁矿 lopolith; magnetic anomaly; structure; ore-prospecting model; Panzhihua vanadium titanomagnetite deposit
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  • 1刘宝君.沉积岩石学[M].北京:地质出版社,1980..

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