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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(ERT,重力分析,μ子成像)的交叉比较

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Muon imaging of volcanoes and of geological structures in general is actively being developed by several groups in the world. It has the potential to provide 3-D density distributions with an accuracy of a few percent. At this stage of development, comparisons with established geophysical methods are useful to validate the method. An experiment has been carried out in 2011 and 2012 on a large trachytic dome, the Puy de D?′me volcano, to perform such a comparison of muon imaging with gravimetric tomography and 2-D electrical resistivity tomography. Here, we present the preliminary results for the last two methods. brbr Northa??south and easta??west resistivity profiles allow us to model the resistivity distribution down to the base of the dome. The modelling of the Bouguer anomaly provides models for the density distribution within the dome that are directly comparable with the results from the muon imaging. Our ultimate goal is to derive a model of the dome using the joint interpretation of all sets of data.
机译:总体上,世界上有几个小组正在积极开发对火山和地质结构进行的μon成像。它有可能提供精度为百分之几的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Trachytic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二维电阻率层析成像。在这里,我们介绍了最后两种方法的初步结果。 Northa ??南和Easta ?? west的电阻率曲线使我们可以建模到圆顶底部的电阻率分布。布格异常的建模提供了圆顶内密度分布的模型,这些模型可直接与μon成像的结果进行比较。我们的最终目标是使用对所有数据集的联合解释来导出圆顶模型。

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