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Numerical simulations of borehole radar detection for metal ore

机译:金属矿石钻孔雷达探测的数值模拟

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We perform finite difference time domain (FDTD) numerical simulation for metal ore detection by borehole radar. The ore-body model is adopted from a practical Ni-Cu-Pt ore body which is a magmatic deposit located in Sudbury, Canada. We design three boreholes along a cross-section perpendicular to the geological strike of the formation which is composed with overburden, ore zone, iron formation, peridotite, granite-gneiss, and sediments. Single-hole measurements within these boreholes are simulated. The simulated data are processed by conventional procedure. We analyzed the simulated borehole radar profiles and found that some interfaces could be detected and some could not, also the ore zone is very absorptive to the wave. By synthetic interpretation of the data from several boreholes, the azimuth ambiguity of the borehole radar could be overcome with some in prior geological information; the geological structure could be delineated exactly. It is inferred that borehole radar is a potential tool for metal ore detection.
机译:我们执行有限差分时域(FDTD)数值模拟,用于通过钻孔雷达探测金属矿石。矿体模型是从位于加拿大萨德伯里的岩浆矿床中的实用镍铜铂矿体中选出的。我们沿垂直于地层地质走向的横截面设计了三个钻孔,该地层由上覆岩层,矿石带,铁层,橄榄岩,花岗岩片麻岩和沉积物组成。模拟了这些钻孔中的单孔测量。模拟数据通过常规程序进行处理。我们分析了模拟的井眼雷达廓线,发现可以检测到某些界面,而不能检测到某些界面,而且矿区对波的吸收性也很高。通过综合解释来自多个井眼的数据,可以通过一些先验的地质信息来克服井眼雷达的方位角模糊性。可以准确地描绘出地质构造。可以推断,钻孔雷达是探测金属矿石的潜在工具。

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