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Rock head elevation model of northern Estonia

机译:爱沙尼亚北部摇滚头海拔模型

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The last rock head elevation model covering the whole of Estonia was compiled about 40 years ago. This model relied on data from 2500 boreholes and excavations and geophysical data. Using the freely accessible present information about more than 34 640 borehole datapoints from the carbonate area, we updated the 40-year-old model. The Devonian sandstone area was disregarded in this work as it needs a different approach of interpolation due to a considerably lower data density and a different behaviour of erosional processes. During this work, the data were filtered for identifying errors and the filtered dataset was interpolated numerous times using the Topo to Raster and Spline methods available in ArcGIS software. The results were compared statistically and by employing the available rock head elevation models. The results from the Topo to Raster method proved to be superior in the correlance next to the partially mapped 1:50 000 rock head elevation model, and the best-suited model was applied to the outcrop area of carbonate rocks in Estonia. Compared to the last rock head elevation model, the new one describes the carbonate bedrock topography in much more detail. It does not match the 1:50 000 scale geological map in all places. possibly due to a much more detailed data set but also because of the errors that may have passed the filtering process during the early stages of work. The rock head elevation model is an important part of GIS-based geological mapping and one of the first steps in producing 3D geological models.
机译:覆盖整个爱沙尼亚的最后一个摇滚头海拔模型大约40年前编制。该模型依赖于2500个钻孔和挖掘和地球物理数据的数据。我们使用来自碳酸盐区的34多个钻孔数据点的自由访问目前信息,我们更新了40岁的型号。由于具有相当低的数据密度和侵蚀过程的不同行为,它在这项工作中忽略了德文扬砂岩区域,因为它需要不同的插值方法。在此工作期间,将筛选数据以识别错误,并且使用Topo将滤波数据集内置了ArcGIS软件中可用的栅格和样条样的栅格和样条曲线方法。结果在统计上进行了比较,并采用可用的摇滚头仰角模型进行比较。 Topo到栅格方法的结果证明是在部分映射的1:50 000摇滚头抬高模型旁边的态度上优越,并且最适合模型应用于爱沙尼亚碳酸盐岩的露头区域。与最后一个摇滚头仰角升降模型相比,新的新型描述了更详细的碳酸碳酸碳酸盐地形。它与所有地方的1:50 000规模地质图不符。可能是由于更详细的数据集,而且由于可能在工作的早期阶段期间通过过滤过程的错误。摇滚头仰角模型是基于GIS的地质映射的重要组成部分,以及生产3D地质模型的第一步之一。

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