SIMULTANEOUS PURE AND SIMPLE SHEAR - THE UNIFYING DEFORMATION MATRIX

被引:185
作者
TIKOFF, B
FOSSEN, H
机构
[1] Department of Geology and Geophysics, University of Minnesota, Minneapolis
关键词
D O I
10.1016/0040-1951(93)90010-H
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Any simultaneous combination of finite simple shear and finite pure shear is a linear transformation which can be expressed as a single transformation matrix. For two dimensions, the matrix is upper triangular with an off-diagonal term, GAMMA, called the effective shear strain. GAMMA is a simple function of the pure and simple shear components. For three dimensions, a simultaneous combination of thrusting in the x direction, thrusting in the y direction, and a wrench in the x direction, in addition to 3 orthogonal components of coaxial strain, can also be represented by a 3 X 3, upper triangular matrix. Here, three off-diagonal terms (GAMMA(xy), GAMMA(xy), and GAMMA(yz)) occur. GAMMA(xy) is a simple function of the horizontal coaxial strain values and thrusting in the x direction, GAMMA(yz) depends on the coaxial strain components in the y and z directions and the thrusting in the y direction, while GAMMA(xz) is related to all six strain components. The matrix also allows for volume change, either homogeneously or preferentially in a single direction. A method of decomposing the deformation matrix into a series of incremental deformation matrices, where each incremental deformation records the same kinematic vorticity number as the finite deformation is shown. The orientation and magnitude of the finite-strain ellipsoid (ellipse) is easily and accurately found at any increment during the deformation.
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页码:267 / 283
页数:17
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