...
首页> 外文期刊>International Journal of Geosciences >Ground Magnetic Survey for the Investigation of Iron Ore Deposit at Oke-Aro in Iseyin East, South-Western Nigeria
【24h】

Ground Magnetic Survey for the Investigation of Iron Ore Deposit at Oke-Aro in Iseyin East, South-Western Nigeria

机译:尼日利亚西南伊塞因东部奥克-阿罗铁矿石矿床调查的地磁测量

获取原文
   

获取外文期刊封面封底 >>

       

摘要

A ground magnetic survey was carried out to investigate the presence of iron ore at a location (Lat. 7.99883° N to Lat. 7.99933° N, Long. 3.57900° E to Long. 3.57990° E) in Iseyin, Oyo State, South - western Nigeria. Ten magnetic traverses each 100 m long at a separation of 5 m were run West-East. Magnetic intensity was taken at intervals of 10 m along each traverse line using the proton precession magnetometer (G-856 AX). The measured magnetic field data were corrected for drift and were presented as profiles. The profiles were interpreted by calculating the depth to the top of anomalies. The data obtained were used to construct magnetic anomaly maps in 2D and 3D. The magnetic survey results delineated this location into some high and low magnetic field intensity regions. The regions of high magnetic field anomaly indicated the presence of materials with high susceptibility which was suspected to be iron compounds. The quantitative and qualitative analyses on interpretations of field data collected were given, while these results provided values for the total component measurements of ground magnetic anomaly that wide ly rang ed between a maximum positive peak result of 8 nT and to a minimum negative peak result of — 6 nT. Using Peter’s half slope technique, depth to the basement was assessed , which actually provide d a maximum depth to basement of 6.25 m. From the knowledge of the geology of the area and also, the magnetic survey employed information, therefore, we can finally conclude that, the study area is under laid by geologic structures which favour the accumulation of iron - ore minerals deposit at Oke - Aro area in Iseyin.
机译:在南部奥西州伊西因(Iseyin)的某个地点(北纬7.99883°至北纬7.99933°,东经3.57900°至东经3.57990°)进行了地磁测量,以调查铁矿石的存在-尼日利亚西部。西向东延伸了10条磁道,每条长100 m,相距5 m。使用质子进动磁力计(G-856 AX)沿每条导线以10 m的间隔获取磁强度。对测得的磁场数据进行漂移校正,并显示为轮廓。通过计算异常顶部的深度来解释剖面。获得的数据用于构建2D和3D中的磁异常图。磁测结果将这个位置划分为一些高磁场强度区域和低磁场强度区域。高磁场异常区域表明存在高敏感性材料,怀疑是铁化合物。给出了对收集的现场数据的解释的定量和定性分析,而这些结果提供了地磁异常总分量测量值,其范围介于最大正峰值结果和最大负峰值结果之间,范围为8 nT。 — 6 nT。使用彼得的半边坡技术,评估了地下室的深度,实际上,地下室的最大深度为6.25 m。因此,从该地区的地质知识以及磁力勘测所利用的信息中,我们最终可以得出结论,该研究区是由有利于Oke-Aro地区铁矿石矿床堆积的地质结构所覆盖。在伊塞因。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号