...
首页> 外文期刊>Earth-Science Reviews: The International Geological Journal Bridging the Gap between Research Articles and Textbooks >Development of structures under the influence of heterogeneous flow field around rigid inclusions: insights from theoretical and numerical models
【24h】

Development of structures under the influence of heterogeneous flow field around rigid inclusions: insights from theoretical and numerical models

机译:刚性包裹体周围异质流场影响下的结构发展:理论和数值模型的启示

获取原文
获取原文并翻译 | 示例
   

获取外文期刊封面封底 >>

       

摘要

Rocks that are mechanically heterogeneous due to the presence of stiff or rigid inclusions floating in a ductile matrix, commonly show a variety of micro- to macro-scale structures developing under the influence of heterogeneous flow field in the neighbourhood of the inclusions. It is of fundamental importance to apprehend the nature of strain heterogeneity around inclusions to understand progressive development of structures associated with rigid inclusions such as strain shadow, foliation drag, porphyroclast mantle, porphyroblast inclusion trails, intragranular fractures, etc. The development of these diverse types of structures can be analyzed with the help of a suitable hydrodynamic theory. In this paper, we review different continuum models that have been proposed to characterize the heterogeneous flow field around rigid inclusions, focusing on recent developments. Recent studies reveal that Jeffery's [Proc. R. Soc. Lond. A 120 (1922) 161.] theory dealing with the motion of ellipsoidal rigid bodies in an infinitely extended viscous medium is more general in nature, and applicable for modeling the heterogeneous flow around both equant and inequant shapes of inclusions and ideal or non-ideal shear deformation of the matrix. The application of this theory, therefore, has advantages over other models, based on Lamb's [Lamb, H., 1932. Hydrodynamics. Cambridge University Press, Cambridge.] theory dealing with spherical inclusions. The review finally illustrates numerical simulations based on hydrodynamic theories, highlighting the controls of physical and kinematic factors on the progressive development of the structures mentioned above. (C) 2002 Elsevier Science B.V. All rights reserved. [References: 85]
机译:由于在韧性基体中漂浮的刚性或刚性夹杂物的存在,机械上是非均质的岩石,通常显示出在夹杂物附近非均质流场的影响下发展出的各种微观到宏观尺度的结构。了解夹杂物周围应变异质性的本质对于理解与刚性夹杂物相关的结构的逐步发展至关重要,例如应变阴影,叶状阻力,卟啉弹性体地幔,成卟啉包裹体痕迹,颗粒内裂缝等。这些类型的发展可以借助适当的流体力学理论来分析结构的数量。在本文中,我们重点研究了最近的发展,提出了不同的连续模型来描述刚性包裹体周围的非均质流场。最近的研究表明,Jeffery的[Proc。 R. Soc。 nd 120(1922)161.]理论涉及无限扩展的粘性介质中的椭圆形刚体的运动,在本质上更为笼统,适用于对包含和不包含在内的相等和不等形状以及理想或非理想状态周围的非均质流动进行建模基质的剪切变形。因此,基于Lamb [Lamb,H.,1932年。流体力学。剑桥大学出版社,剑桥。]关于球形夹杂物的理论。这篇综述最后说明了基于流体动力学理论的数值模拟,重点介绍了物理和运动学因素对上述结构的逐步发展的控制。 (C)2002 Elsevier Science B.V.保留所有权利。 [参考:85]

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号