利用航磁资料对Kebbi州南部金矿化潜力进行地球物理评价

Pub Date : 2022-06-10 DOI:10.7494/geol.2022.48.2.177
Abdulrahaman Idris Augie, K. Salako, Adewuyi Abdulwaheed Rafiu, M. O. Jimoh
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引用次数: 2

摘要

分析了Kebbi州南部及其周边地区的磁特征,并结合该地区的地质背景,圈定了可能存在金矿化的构造。所使用的航磁数据是2005年至2010年由辉固航空调查公司代表尼日利亚联邦政府进行的调查。将赤道还原(RTE)、一阶和二阶垂直导数(FVD和SVD)、勘探定位中心(CET)、分析信号(AS)、源参数成像(SPI)和倾斜导数(TDR)技术应用于覆盖该区域的磁数据。AS技术结果显示,研究区具有高振幅磁异常(大于0.048 nT/m)的特征,这些异常可能是铁磁性矿物,如金。FVD、SVD、CET和TDR技术也有助于描绘被认为与蚀变带有关的轮廓(如断层、断裂或剪切带),这些蚀变带在确定金矿化带中起着重要作用。这些地物/地貌的取向方向呈北东—西南向。所圈定的断层、断裂或剪切带代表可能的矿化脉。利用SPI算法发现病原体的发生深度在137 m以下。区域内圈定的构造与区域地质背景相比较,对应于石英云母片岩、花岗岩、黑云母、片麻岩、闪长岩、中粗粒花岗岩和黑云母角闪石花岗岩。这些技术的结果揭示了可能含金的蚀变带。这些地区对应于以下地区:优里和尚加的东南部、法凯、恩加斯基、祖鲁、马加马、里饶以及瓦萨古/丹科和布库尤姆的东部。
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Geophysical assessment for gold mineralization potential over the southern part of Kebbi State using aeromagnetic data
The magnetic signatures over the southern part of Kebbi State and its environs were analyzed together with the geological settings of the area to delineate the structures that may host gold mineralization. The aeromagnetic data used was the survey carried out by Fugro airborne surveys between 2005 and 2010 on behalf of the Federal Government of Nigeria. The reduction to equator (RTE), first and second vertical derivatives (FVD and SVD), Centre for Exploration Targeting (CET), analytic signal (AS), source parameter imaging (SPI) and tilt derivative (TDR) techniques were applied to the magnetic data covering the area. The results of the AS technique revealed that the study area is characterized with high amplitudes of magnetic anomalies (above 0.048 nT/m) and these could be of ferromagnetic minerals such as gold. The FVD, SVD, CET and TDR techniques also helped in delineating the lineaments (such as faults, fractures or shears zones) believed to be associated with alteration zones which play an important role in determining gold mineralized zones. The direction of the orientation of these features/lineaments trended in the NE-SW direction. The faults, fractures or shears zones delineated represent veins of possible mineralization. The depth of occurrence to the causative bodies using SPI algorithms was found to be below 137 m. Structures delineated within the area, when compared with the geological setting of the area, correspond to quartz-mica schist, granite, biotite, gneiss, diorite, medium coarse-grained and biotite hornblende granite. Results from these techniques revealed alteration zones that may host gold. These regions correspond to the following areas: SE parts of Yauri and Shanga, Fakai, Ngaski, Zuru, Magama, Rijau, and the eastern part of Wasagu/Danko and Bukkuyum.
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