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作 者:高秀鹤 于长春 李行素 葛藤菲 何敬梓 GAO Xiuhe;YU Changchun;LI Xingsu;GE Tengfei;HE Jingzi(China Aero Geophysical Survey and Remote Sensing Center for Natural Resources,Beijing 100083,China)
机构地区:[1]中国自然资源航空物探遥感中心,北京100083
出 处:《现代地质》2024年第1期25-34,共10页Geoscience
基 金:国家重点研发计划项目(2022YFC2903704,2017YFC0602201);国家自然科学基金项目(42004125)。
摘 要:深部磁铁矿体的埋深较大,且目标矿体和成矿岩体产生的磁异常往往相互耦合、干扰,加之航磁测量的观测面高,导致深源矿致航磁异常的信号一般较弱。因此,难以从原始航磁异常图中直接圈定深部磁铁矿靶区。位场分离技术是提取矿致异常的有效途径,但位场分离方法众多,且使用便捷性、提取效果存在差异,筛选适用于深部磁铁矿的矿致异常提取方法以及讨论相关参数调节方法具有较大的理论和实用价值。本文对比研究了6种常用的位场分离方法,分析了各方法参数调节的便捷性和有效性。通过模型试验,从全区和靶区两个尺度对比了各方法对矿致异常的提取效果。山东齐河—禹城厚覆盖区的深部赋存接触交代成因的磁铁矿床,是深部矿产的典型代表,本文根据该区地质模型建立理论磁性模型,验证了深部矿致异常提取的可行性。实测数据处理部分,提出基于标志剖面交互调节相关参数以及验证矿致异常提取效果,最终提取的矿致异常结果与已知的钻孔见矿信息匹配,表明该结果与实际的矿致异常相关性较高,可为后续矿体靶区圈定和钻孔位置布设提供参考。The large depth that the magnetite is buried and the long distance of aeromagnetic survey always leads to a weak signal of magnetic anomaly.In addition,due to that the deep magnetite mostly is formed through contact metasomatism caused by magmatic intrusion,the magnetic anomalies sourced from the source rocks and orebodies are always coupled and interfered with each other.This is challenging to directly delineate the target area for the deep magnetite orebody from the original map of aeromagnetic anomaly.Previous studies show that potential field separation technology is an effective approach to extract ore-caused anomalies.However,there are many potential field separation methods and they are all different,in terms of operation convenience and different results of extraction.In this paper,we systematically compared and analyzed the convenience of six commonly used separation methods,and evaluated the effects of extracting ore-caused anomalies from both the whole and target regions.Consequently,we established the theoretical model and verified the feasibility extracting the deep ore-caused anomalies based on the geologic background of the Qihe area,Shandong.At the end,we recommend using the marker profile line to verify the extraction effect of ore-induced anomalies when the measured data were processed.The ore-caused anomalies extracted agree with the known drilling data,indicating a strong correlation between the extracted and realistic anomalies.This study provides a reference for future delineation of target ore fields and laying-out of drilling locations.
分 类 号:P318.63[天文地球—固体地球物理学]
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