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首页> 外文期刊>International Journal of Geophysics >Determination of Location and Depth of Mineral Rocks at Olode Village in Ibadan, Oyo State, Nigeria, Using Geophysical Methods
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Determination of Location and Depth of Mineral Rocks at Olode Village in Ibadan, Oyo State, Nigeria, Using Geophysical Methods

机译:利用地球物理方法确定尼日利亚奥约州伊巴丹奥洛德村矿物岩的位置和深度

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Magnetic and resistivity geophysical methods were used to investigate the location and depth of mineral rocks at Olode village, Oyo State, Nigeria. 80 magnetic data points were acquired in 10 profiles using G-816 proton precession magnetometer with 10 m spacing in between each profiles and 10 m stations interval. After correcting diurnal variations, the raw magnetic data obtained were plotted as 2D and 3D magnetic contour maps. The residual anomalies obtained were plotted against distance using Microsoft Excel, and Peter’s half-slope method was used to find the depth to the magnetic sources. The magnetic signature obtained show considerable varying amplitude from a minimum value of 155.3 nT at a depth of 6.37 m to a maximum value of 670.3 nT at a depth of 6.25 m. Resistivity data were obtained using Campus Tiger resistivity meter and 9 VESs were acquired using Schlumberger configuration. All VESs were 150 m long, 75 m on each side of the referenced points which were 10 m apart. VESs 1–4 and 7–9 are underlined with rocks of high conductivity and susceptibility values. VESs 5 and 6 show rocks with low conductivity and susceptibility values. The results of these geophysical methods show that there are rocks with high magnetic susceptibility and conductivity values from the centre towards the eastern region of the study area and low magnetic susceptibility and conductivity values at the western region. On the average, the depths of these rocks from the surface fall in the interval of 5.80 m to 6.72 m.
机译:磁性和电阻率地球物理方法被用于调查尼日利亚奥约州奥洛德村矿物岩的位置和深度。使用G-816质子进动磁力计在10个剖面中采集了80个磁数据点,每个剖面之间的间隔为10μm,测站间隔为10μm。校正昼夜变化后,将获得的原始磁数据绘制为2D和3D磁轮廓图。使用Microsoft Excel将获得的残余异常相对于距离作图,并使用Peter的半坡度法找到距磁源的深度。所获得的磁签名显示出相当大的幅度变化,从在6.37μm深度处的最小值155.3 nT到在6.25μm深度处的最大值670.3 nT。使用Campus Tiger电阻率仪获得电阻率数据,并使用Schlumberger配置获得9 VES。所有VES的长度均为150µm,参考点的每一侧均为75µm,相距10µm。 VES 1–4和VES 7–9带有高电导率和磁化率值的岩石。 VES 5和6显示出具有低电导率和磁化率值的岩石。这些地球物理方法的结果表明,从研究区域的中心到东部地区,岩石的磁化率和电导率值高,而西部地区的磁化率和电导率值低。平均而言,这些岩石从地表的深度介于5.80 m至6.72 m之间。

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