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首页> 外文期刊>Geoscientific Instrumentation, Methods and Data Systems >Inner structure of the Puy de D?me volcano: cross-comparison of geophysical models (ERT, gravimetry, muon imaging)
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Inner structure of the Puy de D?me volcano: cross-comparison of geophysical models (ERT, gravimetry, muon imaging)

机译:Puy de D?me火山的内部结构:地球物理模型的相互比较(ERT,重量分析,μ子成像)

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Muon imaging of volcanoes and of geological structures in general isactively being developed by several groups in the world. It has the potential toprovide 3-D density distributions with an accuracy of a few percent. At thisstage of development, comparisons with established geophysical methods areuseful to validate the method. An experiment has been carried out in 2011and 2012 on a large trachytic dome, the Puy de D?me volcano, to performsuch a comparison of muon imaging with gravimetric tomography and 2-Delectrical resistivity tomography. Here, we present the preliminary resultsfor the last two methods.North–south and east–west resistivity profiles allow us to model theresistivity distribution down to the base of the dome. The modelling of theBouguer anomaly provides models for the density distribution within the domethat are directly comparable with the results from the muon imaging. Ourultimate goal is to derive a model of the dome using the jointinterpretation of all sets of data.
机译:总体上,世界上有几个小组正在积极开发火山和地质结构的μ相影像。它有可能以百分之几的精度提供3-D密度分布。在开发的这一阶段,与已建立的地球物理方法进行比较有助于验证该方法。 2011年和2012年,在大型的Trachy圆顶Puy de D?me火山上进行了一项实验,以比较μ子成像与重量层析成像和2-D电阻率层析成像。在这里,我们介绍了最后两种方法的初步结果。 南北和东西方向的电阻率曲线使我们可以建模直至圆顶底部的电阻率分布。布格异常的建模为模型中的密度分布提供了模型,可直接与μ子成像结果进行比较。我们的最终目标是使用所有数据集的联合解释来导出圆顶模型。

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