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Glacial stress field orientation reconstructedthrough micromorphology and pX-ray computedtomography of till

机译:冰川应力场取向重建重建微晶和PX射线计算为直到直到

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Detailed laboratory analyses largely support field studies on the petrology of glacial materials. Inparticular, detailed structural analysis of glacial sediments helps reconstruct the presence, orienta-tion and intensity of glacial stress fields. This pilot study compares thin-section micromorphology(two-dimensional observation under a microscope) and |ìX-ray computed tomography (|ìXR-CT,three-dimensional observation involving data collection and subsequent processing) to evaluate thepotential of the latter technique to yield reliable data. The location and stratigraphy of samplingsites are reported for a complete presentation. Results are encouraging: compared with thin-section micromorphology, pX-ray computed tomography yielded results that are more detailed,reproducible and unaffected by cutting orientation. Moreover, |ìXR-CT is easily applied to inco-herent materials, brittle samples and unique specimens.
机译:详细的实验室分析了很大程度上支持冰川材料岩石学的现场研究。冰川沉积物的不具体化的结构分析有助于重建冰川应力场的存在,东方和强度。该试点研究比较了薄截面微晶(显微镜下的二维观察)和|ì射线计算机断层扫描(|ìXR-CT,三维观察,涉及数据收集和随后的处理),以评估后一种技术的屈服可靠的数据。据报道,类别的位置和地层是完整的演示。结果令人鼓舞:与薄截面微晶相比,PX射线计算断层扫描产生的结果更详细,可再现,不受切割方向的影响。此外,|ìXR-CT容易施加到凝固材料,脆性样品和独特的标本。

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