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Development of quartz c-axis crossed/single girdles under simple-pure shear deformation: Results of visco-plastic self-consistent modeling

机译:简单纯剪切变形下石英c轴交叉/单腰带的发展:粘塑性自洽模型的结果

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摘要

Quartz c-axis fabrics are widely used to determine the shear plane in ductile shear zones, based upon an assumption that the shear plane is perpendicular to both the central segment of quartz c-axis crossed girdle and single girdle. In this paper the development of quartz c-axis fabric under simple-pure shear deformation is simulated using the visco-plastic self-consistent (VPSC) model so as to re-examine this assumption. In the case of no or weak dynamic recrystallization, the simulated crossed girdles have a central segment perpendicular or nearly perpendicular to the maximum principal finite strain direction (X) and the XY finite strain plane, and at a variable angle relative to the imposed kinematic framework that is dependent on the modeled flow vorticity and finite strain. These crossed girdles have a symmetrical skeleton with respect to the finite strain axes, regardless of the bulk strain and the kinematic vorticity, and rotate in a way similar to the shear sense with increasing bulk strain ratio. The larger the vorticity number the more asymmetrical their legs tend to be. In the case of strong dynamic recrystallization and large bulk strain, under simple shear the crossed girdle switches into single girdles, sub-perpendicular to the shear plane, by losing the weak legs. The numerical results in our models do not confirm the above-mentioned assumption.
机译:基于剪切平面既垂直于石英c轴交叉腰带和单个腰带的中心段的假设,石英c轴织物也广泛用于确定韧性剪切区域中的剪切平面。在本文中,使用粘塑性自洽(VPSC)模型模拟​​了简单纯剪切变形下石英c轴织物的发展,从而重新检验了这一假设。在没有或没有弱的动态再结晶的情况下,模拟的交叉带具有垂直于或几乎垂直于最大主有限应变方向(X)和XY有限应变平面的中心线段,并且相对于施加的运动学框架具有可变的角度这取决于模型的流动涡度和有限应变。不管整体应变和运动涡度如何,这些交叉的腰带都具有关于有限应变轴的对称骨架,并且随着整体应变比的增加,以类似于剪切的方式旋转。旋涡数越大,其腿部倾向于越不对称。在强动态再结晶和大体积应变的情况下,在简单剪力作用下,交叉的腰带会失去弱腿,从而变成垂直于剪切平面的单个腰带。我们模型中的数值结果不能证实上述假设。

著录项

  • 来源
    《Journal of structural geology》 |2014年第9期|261-270|共10页
  • 作者

    Guanjun Nie; Yehua Shan;

  • 作者单位

    Lab of Marginal Sea Geology, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China,Graduate University of Chinese Academy of Sciences, Beijing 100039, China;

    Lab of Marginal Sea Geology, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Quartz c-axes; Girdle; Shear plane; Non-coaxial deformation; VPSC model;

    机译:石英c轴带;剪切机非同轴变形;VPSC模型;
  • 入库时间 2022-08-18 03:37:16

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