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A Multiscale Numerical Modeling Investigation on the Significance of Flow Partitioning for the Development of Quartz c-Axis Fabrics

机译:石英C轴织物开发流量分区意义的多尺度数值模型调查

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Quartz c-axis fabrics in natural mylonites can vary to such an extent that they apparently give opposite senses of shear in a single thin section. Many hypotheses have been invoked to explain this. Here, we couple our self-consistent multiscale approach for flow partitioning with the viscoplastic self-consistent model for c-axis fabric simulation to investigate quartz c-axis fabric development. Quartz aggregates are regarded as microscale Eshelby inhomogeneities embedded in a macroscale medium whose effective rheology is represented by a hypothetical homogeneous equivalent medium which is assumed to be rheologically isotropic or has a planar anisotropy. We reproduced the observed quartz c-axis fabrics. We found that although the microscale flow fields are distinct from one another and from the macroscale flow, the microscale vorticity in every inhomogeneity has the same sense as the macroscale vorticity. This implies that one can use the average of the microscale vorticity axes determined through the crystallographic vorticity axis analysis to obtain the macroscale vorticity axis. However, quartz c-axis fabrics cannot be used to determine the vorticity number where flow partitioning is significant.
机译:天然糜棱岩中的石英c轴组构可能会发生变化,以至于在单个薄片中,它们显然会产生相反的剪切感。许多假说被用来解释这一点。在这里,我们将自洽多尺度流动划分方法与粘塑性自洽模型相结合,用于c轴组构模拟,以研究石英c轴组构的发展。石英骨料被视为嵌入宏观介质中的微尺度Eshelby不均匀体,其有效流变性由假设为流变各向同性或具有平面各向异性的均质等效介质表示。我们复制了观察到的石英c轴组构。我们发现,尽管微尺度流场彼此不同,也不同于宏观尺度流场,但每个非均匀性中的微尺度涡度与宏观涡度具有相同的意义。这意味着可以使用通过晶体涡度轴分析确定的微尺度涡度轴的平均值来获得宏观涡度轴。然而,石英c轴组构不能用于确定流动分配显著的涡度数。

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