Page 84 - Statistics and Data Analysis in Geology
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Statistics and Data Analysis in  Geology-  Chapter 3

             point in a positive coordinate direction, or both components point in a negative
             coordinate direction. Otherwise, the shear stress is negative. In order for the cube
             to be in rotational equilibrium, shear stresses on adjacent faces must balance; so,
             for example, uxy = urx. This means that the stress matrix is symmetric about the
             diagonal:








             Turcotte and Schubert (1982) provide a more detailed discussion of  stress in the
             subsurface and the measurement of stress components.
                 By finding the eigenvalues and eigenvectors of  the 3 x 3 stress matrix, we can
             rotate the imaginary cube into a coordinate system in which all the shear stresses
             will be zero.  The eigenvalues represent the magnitudes of  the three orthogonal
             stresses. Their associated eigenvectors point in the directions of the stresses. The
             largest eigenvalue, hl, represents the maximum normal stress and the smallest,
             h3, represents the minimum normal stress. The maximum shear stress is given by
              (Al  - h3)/2 and occurs along a plane oriented perpendicular to a line that bisects
              the angle between the directions of  maximum and minimum normal stress (that
             is, between the first and third eigenvectors). In a homogenous, isotropic material,
             failure (te., faulting) will tend to occur along this plane. The orientation of this plane
              can be determined from the elements of  the first eigenvector. In the conventional
             notation used by geologists, the strike of the first eigenvector is tan-l  (Y~z/YI~)
              and its dip is






              (Here,  Vij refers to the jth element of the ith eigenvector.) The strike and dip of the
              second and third eigenvectors can be found in the same manner.
                  Three-dimensional stress measurements have been made in a pillar in a deep
             mine, yielding the following stress matrix:

                                                            1
                                           61.2    4.1  -8.2
                                            4.1  51.5  -3.0
                                           -8.2   -3.0  32.3



              The data are given in megapascals (MPa) and were recorded by strain gauges placed
              so the measurements have the same orientation as our imaginary cube (X increasing
              to the east, Y to the north, and Z increasing upward). Find the principal stresses
              and their associated directions. What is the maximum shear stress and what is the
              strike and dip of  the plane on which this stress occurs?





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