An overdetermined linear inverse problem is expressed as \( Gm = d \), where \( G \) is the data kernel, \( m \) is the vector of model parameters and \( d \) is the vector of observed data. If damping is applied to the inverse problem and the resultant generalized inverse is represented by \( G^{-g} \), the \textbf{model resolution matrix can be expressed as:}
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In inverse theory, the model resolution matrix is always expressed as \( R_m = G^{-g} G \), while the data resolution matrix is \( R_d = G G^{-g} \). Remember: model resolution involves \( G^{-g} G \).
Step 1: General inverse solution
For the linear inverse problem:
\[
Gm = d
\]
the solution is obtained using a generalized inverse \( G^{-g} \):
\[
m = G^{-g} d
\]
Step 2: Define estimated model parameters
The estimated model parameters are written as:
\[
m_{\text{est}} = G^{-g} d
\]
Since the observed data is \( d = G m \):
\[
m_{\text{est}} = G^{-g} G m
\]
Step 3: Model resolution matrix
The model resolution matrix \( R_m \) is defined as:
\[
m_{\text{est}} = R_m \, m
\]
Comparing with the above, we have:
\[
R_m = G^{-g} G
\]
Step 4: Interpretation
- The resolution matrix measures how well the true model \( m \) can be recovered from the estimated solution.
- An ideal resolution matrix is the identity matrix \( I \), but in practice, due to noise and damping, it deviates from \( I \).
\[
\boxed{R_m = G^{-g} G}
\]