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Analysis and interpretation of GPR datasets for integrated archaeological mapping

机译:用于综合考古制图的GPR数据集的分析和解释

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An integrated approach to ground-penetrating radar interpretation should include not only the standard amplitude slice maps and isosurface renderings but also an analysis of individual reflection traces and adjusted and processed reflection profiles. Only when all those basic datasets are interpreted can the plethora of reflection features at various depths and locations within a grid be understood, especially in complex geological and archaeological settings. Topographically adjusted profiles can provide important clues to changes in reflectivity along a transect, indicating why certain amplitude features are visible (or not) in slice maps. An integration of excavation and outcrop data with reflection profiles can often indicate what features are producing high-amplitude reflections and which are yielding no reflection at all. Even individual reflection traces can be studied for polarity changes, which can help in identifying the types of buried materials that are producing reflections. All these datasets, some of which are often overlooked, must be integrated during interpretation, especially in complicated ground conditions.
机译:探地雷达解释的综合方法不仅应包括标准幅度切片图和等值面渲染,而且还应包括对单个反射轨迹以及经过调整和处理后的反射轮廓的分析。只有解释了所有这些基本数据集后,才能理解网格内各种深度和位置的过多反射特征,尤其是在复杂的地质和考古环境中。地形调整后的轮廓可以为沿样条线的反射率变化提供重要线索,表明为什么某些幅值特征在切片图中可见(或不可见)。开挖和露头数据与反射剖面的集成通常可以指示哪些特征正在产生高振幅反射,哪些特征根本不产生反射。甚至可以研究单个反射迹线的极性变化,这有助于确定产生反射的掩埋材料的类型。所有这些数据集,其中一些经常被忽略,必须在解释过程中加以整合,特别是在复杂的地面条件下。

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