地电法在岩斑岩沉降物表征中的应用

A. As, Dikedi Pn, Oghar, ukun Mo
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引用次数: 1

摘要

研究工作的重点是在Obrubra地区Iyamitet定居点内划定重晶石-方铅矿沉积物。由于尼日利亚和世界经济越来越需要从矿物矿石收益中获得资金,作为区域和全球收入的另一种来源,目前的工作变得必要。矿石具有一定的全球经济价值和重要性。在划定矿藏所在区域时,采用一对电流电极将地电引入地下,同时通过插入另一对电位电极测量电压。采用斯伦贝谢阵列和垂直电测深(VES)技术测量被测地下视电阻率。分别生成了18条垂直电测深曲线、5条地质剖面、5张等电阻率图和4张等等层图。由于矿石(重晶石和方铅矿)位于寄主岩石中,18个表中所示的18个电测深结果显示了这些矿石的不同深度——以及容纳它们的岩石。在等电阻率图中,红色斑块的电阻率超过1000 Ωm表明,根据取心和钻孔信息,重晶石的潜力与(10-15)m的不同深度相吻合。等距图中最浅的斑块代表调查区域的最高海拔。深蓝色区域代表被调查区域的最低部分。虽然结果没有显示方铅矿矿石物质的存在,但可能是多次矿石侵入破坏了方铅矿的电阻率读数;方铅矿的存在可以通过结合多种地球物理技术的结果来发现
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Adopting Geo-electric Approach in Mineral Characterization of Iyamitet Settlement
The research work epicenters on the delineation of Barite-Galena sediments within Iyamitet settlement of Obrubra region, Present work has become necessary owing to the growing need for the Nigeria and indeed world economy to be funded from proceeds of mineral ores as an alternative source of regional and global revenues. The ore garners some global economic value and importance. In delineating the region which habours the mineral ore, geo-electricity was introduced into the subsurface by employing a pair of current electrodes while the voltage is measured by inserting another pair of potential electrodes. Shlumberger array and Vertical Electrical Sounding (VES) techniques were adopted to measure apparent ground resistivity of the subsurface under investigation. Eighteen Vertical Electrical Sounding Curves, five geo-sections, five Isoresistivity and four Isopach maps were generated respectively. Since mineral-ores (Barite and Galena) are located within the host rocks, all 18 VES results represented in 18 tables show varied depths to these ores--and the rocks which harbours them.. The Iso-resistivity map with red patches bearing resistivities over 1000 Ωm demonstrates potential for Barite which coincide with varying depth of (10-15) m as revealed by the coring and borehole information. The Iso-pach map with the lightest patch represents highest altitude of the area under investigation. The dark blue patch represents the lowest portion of the region under investigation. Though results do not show the presence of Galena ore material, it is possible that multiple ore intrusions could have compromised the resistivity reading of Galena; Galena presence could be uncovered by combining outcome of results from multiple geophysical techniques
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