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Deep exploration using long-offset transient electromagnetics: interpretation of field data in time and frequency domain

机译:使用长偏移瞬态电磁学的深度探索:时间和频域中现场数据的解释

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摘要

In the framework of the Deep Electromagnetic Soundings for Mineral Exploration project, we conducted ground-based long-offset transient-electromagnetic measurements in a former mining area in eastern Thuringia, Germany. The large-scale survey resulted in an extensive dataset acquired with multiple high-power transmitters and a high number of electric and magnetic field receivers. The recorded data exhibit a high data quality over several decades of time and orders of magnitude. Although the obtained subsurface models indicate a strong multi-dimensional subsurface with variations in resistivity over three orders of magnitude, the electrical field step-on transients are well fitted using a conventional one-dimensional inversion. Due to superimposed induced polarization effects, the transient step-off data are not interpretable with conventional electromagnetic inversion. For further interpretation in one and two dimensions, a new approach to evaluate the long-offset transient-electromagnetic data in frequency domain is realized. We present a detailed workflow for data processing in both domains and give an overview of technical obstructions that can occur in one domain or the other. The derived one-dimensional inversion models of frequency-domain data show strong multi-dimensional effects and are well comparable with the conventional time domain inversion results. To adequately interpret the data, a 2.5D frequency-domain inversion using the open source algorithm MARE2DEM (Modeling with Adaptively Refined Elements for 2-D EM) is carried out. The inversion leads to a consistent subsurface model with shallow and deep conductive structures, which are confirmed by geology and additional geophysical surveys.
机译:在矿物勘探项目深度电磁探测的框架中,我们在德国东部的前矿区进行了基础的长偏移瞬态电磁测量。大规模调查导致具有多个高功率发射器和大量电磁场接收器获取的广泛数据集。记录的数据在数十年的时间和数量级的几十年中表现出高数据质量。尽管所获得的地下模型表示强的多维地下,其具有超过三个级比的电阻率的变化,但是使用传统的一维反转井井有素地拟合电场踩踏瞬态。由于升高的辐射偏振效应,瞬态降级数据不能与传统的电磁反转解释。为了进一步解释一个和两个维度,实现了评估频域中的长偏移瞬态电磁数据的新方法。我们在两个域中提供了一个详细的工作流程,以便在两个域中进行数据处理,并概述在一个域或另一个域中可能发生的技术障碍物。频率域数据的导出的一维反演模型显示出强的多维效果,并且与传统的时域反转结果相当。为了充分解释数据,执行使用开源算法MARE2DEM的2.5D频域反转(使用适用于2-D EM的自适应细化元件)。反演导致具有浅和深的导电结构的一致地下模型,由地质和地层进行确认。

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