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principles and applications of microearthquake networks

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110 5. Inversion <strong>and</strong> Optimization<br />

then the eigenvalue problem for AT becomes<br />

(5.19) ATV = VA<br />

Let us take the transpose on both sides <strong>of</strong> Eq. (5.19)<br />

(5.20) VTA = AVT<br />

<strong>and</strong> let us postmultiply this equation by U<br />

(5.21) VTAU = AVW<br />

On the other h<strong>and</strong>, let us premultiply both sides <strong>of</strong> Eq. (5.16) by VT<br />

(5.22) VTAU = VTJA<br />

Because the left-h<strong>and</strong> sides <strong>of</strong> Eq. (5.21) <strong>and</strong> Eq. (5.22) are equal, we<br />

obtain<br />

(5.23) AVTU = VTUA<br />

Let us denote the product VTU by W, whose elements are W, <strong>and</strong> write<br />

out Eq. (5.23)<br />

(5.24) =o<br />

If it is assumed that the eigenvalues are distinct, we obtain W, = 0 for<br />

i #j. This proves that VT <strong>and</strong> U are orthogonal. Since the length <strong>of</strong><br />

eigenvectors is arbitrary, we may choose VTU = I, where I is the identity<br />

matrix. Thus, we have<br />

(5.25) VT = U-I, V = (UT)-'; U = (VT-', UT = V-'<br />

We are now in a position to derive the fundamental decomposition<br />

theorem. If we postmultiply Eq. (5.16) by VT, we have<br />

(5.26) AUVT = UAVT<br />

In view <strong>of</strong> Eq. (5.25), UVT = I, so that<br />

(5.27) A = UAVT<br />

Equation (5.27) shows that any n x n matrix A with distinct eigenvalues is<br />

obtainable by multiplying three matrices together, namely, the matrix U<br />

with the eigenvectors <strong>of</strong> A as columns, the diagonal matrix A with the

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