A general deformation matrix for three-dimensions

被引:13
作者
Soto, JI [1 ]
机构
[1] UNIV GRANADA,FAC SCI,DEPT GEODINAM,CSIC,GRANADA 18008,SPAIN
来源
MATHEMATICAL GEOLOGY | 1997年 / 29卷 / 01期
关键词
simple shear; coaxial progressive deformation; velocity gradient tensor; deformation tensor; vorticity tensor; strain ellipsoid; passive linear marker;
D O I
10.1007/BF02769621
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
A deformation that is obtained by any simultaneous combination of two steady-stare progressive deformations: simple shearing and a coaxial progressive deformation, involving or not a volume change, can be expressed by a single transformation, or deformation matrix. In the general situation of simple shearing in a direction non-orthogonal with the principal strains of the coaxial progressive deformation, this deformation matrix is a function of the strain components and the orientation of shearing. In this example, two coordinate systems are defined: one for the coaxial progressive deformation (x(i) system), where the principal and intermediate strains are two horizontal coordinate axes, and another for the simple shear (x(i)' system), with any orientation in space. For steady-state progressive deformations, from the direction cosines matrix that defines the orientation of shear strains in the x(i) coordinate system, an asymmetric finite-deformation matrix is derived. From this deformation matrix, the orientation and ellipticity of the strain ellipse, or the strain ellipsoid for three-dimensional deformations, carl be determined. This deformation matrix also can be described as a combination of a rigid-body rotation and a stretching represented by a general coaxial progressive deformation. The kinematic vorticity number (W-k) is derived for the general deformation matrix to characterize the non-coaxiality of the three-dimensional deformation. An application of the deformation matrix concept is given as an example, analyzing the changes in orientation and stretching that variously-oriented passive linear markers undergo after a general two-dimensional deformation. The influence of the kinematic vorticity number, the simple and pure shear strains, and the obliquity between the two deformation components, on the linear marker distribution after deformation is discussed.
引用
收藏
页码:93 / 130
页数:38
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