Augmenting 1D conductivity depth sections to include information pertaining to 2D/3D conductors

M. Combrinck
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Abstract

Summary Conductivity depth data presentations derived using 1D approximations have become a very popular way to present airborne electromagnetic (AEM) data. While data profiles and a single error limit per station can accompany these presentations there are more information contained in data. This work proposes some ideas for augmenting 1D derived data presentations to highlight two and three-dimensional conductors as well as more detailed error level indication. The 1D conductivity depth algorithm used is an extended version of the S-layer differential transform. The depths calculated with the transform is used also present decay constant values corrected for conductive background responses. Fraser filtered X-component data are used to indicate structural complexity and data fit error levels are used to grey out areas on the depth section presentations where the results are less reliable. To demonstrate these ideas a line of Xcite data over the Abra deposit in Western Australia is analysed. The augmentations add valuable information to the conductivity depth section in the sense of drawing attention the where the 1D assumptions are not valid and should encourage interpreters to pursue 2D or 3D modelling techniques for successfully mapping the ore deposit.
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增加1D电导率深度剖面,包括有关2D/3D导体的信息
利用一维近似导出的电导率深度数据表示已经成为一种非常流行的表示机载电磁(AEM)数据的方法。虽然数据概要和每个站点的单一错误限制可以伴随这些演示,但数据中包含的信息更多。这项工作提出了一些想法,以增加一维衍生数据的表现,以突出二维和三维导体,以及更详细的误差水平指示。使用的一维电导率深度算法是s层微分变换的扩展版本。用变换计算的深度也用于根据导电背景响应校正的衰减常数值。Fraser过滤的x分量数据用于表示结构复杂性,数据拟合误差级别用于灰色化深度剖面表示中结果不太可靠的区域。为了证明这些观点,我们分析了西澳大利亚州Abra矿床上的一系列Xcite数据。这些扩展为电导率深度剖面增加了有价值的信息,引起了人们对一维假设无效的注意,并应鼓励解释人员采用2D或3D建模技术来成功地绘制矿床。
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