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首页> 外文期刊>Journal of structural geology >The application of high resolution X-ray computed tomography on naturally deformed rock salt: Multi-scale investigations of the structural inventory
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The application of high resolution X-ray computed tomography on naturally deformed rock salt: Multi-scale investigations of the structural inventory

机译:高分辨率X射线计算机断层摄影术在自然变形岩盐上的应用:结构清单的多尺度研究

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X-ray computed tomography (CT) represents a useful technique providing new perspectives and insights for the structural investigation of naturally-deformed rock salt. Several samples of Permian rock salt from Gorleben, Asse and Teutschenthal (Germany) were investigated by exploiting the non-destructive nature of mu CT and nCT techniques particularly for salt rocks. CT imaging enabled the visualization and quantification of anhydrite impurities, pore space and fluid phases located along grain-boundaries or trapped as intracrystalline inclusions. Disseminated grains and aggregates of anhydrite in rock salt of the Gorleben salt dome have been visualized and quantified by mu CT for the first time in order to portray their spatial occurrence. The visualization of anhydrite aggregates and pore space shows no correlation between their spatial distributions. This independence excludes the anhydrite to be responsible for elevated porosity (0.87 +/- 0.07 vol.-%). High-resolution nCT scans (<= 1 mu m voxel size) of single intracrystalline and grain-boundary fluid inclusions from Gorleben and Asse rock salt allowed the visualization and quantification of their various phase components. A major achievement is the detailed description of the morphology and shape of the fluid inclusions and of their phase components, which has not been conducted in rock salt research by high-resolution X-ray CT imaging before. (C) 2015 Elsevier Ltd. All rights reserved.
机译:X射线计算机断层扫描(CT)代表了一种有用的技术,可为自然变形岩盐的结构研究提供新的观点和见识。通过利用mu CT和nCT技术的无损性质,尤其是盐岩,研究了来自Gorleben,Asse和Teutschenthal(德国)的二叠纪岩盐的一些样品。 CT成像可以直观地观察和量化沿晶界或被捕获为晶体内夹杂物的硬石膏杂质,孔隙空间和流体相。 mu CT首次可视化并定量了戈尔本盐穹顶岩盐中散布的硬石膏和粒状硬石膏,以描绘其空间分布。硬石膏聚集体和孔隙空间的可视化显示它们的空间分布之间没有相关性。这种独立性排除了硬石膏导致孔隙率升高(0.87 +/- 0.07 vol .-%)的原因。对来自Gorleben和Asse岩盐的单个晶体内和晶界流体包裹体进行高分辨率nCT扫描(<= 1微米体素尺寸)可以可视化和量化其各种相成分。一项重大成就是详细描述了流体包裹体的形态和形状以及它们的相组成,这在以前的岩盐研究中尚未通过高分辨率X射线CT成像进行过描述。 (C)2015 Elsevier Ltd.保留所有权利。

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