Geophysical Signal Analysis

By E. Robinson, S. Treitel. 2000

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Amplitude and kinematic corrections of migrated images for nonunitary imaging operators (2004, background): “Hence, I can rewrite equation (9) such that the matrix B becomes a vector and m 2 becomes a convolution matrix (Robinson and Treitel, 1980): m 1 = M 2 b. (10”
Adaptive subtraction of multiples using the L1‐norm (2004, methodology): “As stated before, the IRLS method used becomes more efficient in the case of L2-norm subtraction (twice as fast) but is still 5–10 times slower than a conventional linear least-squares algorithm using the Levinson scheme (see e.g. Robinson and Treitel 1980).”
Through wall imaging: Historical perspective and future directions (2008, neutral): “As examples, geophysical imaging techniques generally measure seismic propagation through the earth to look for discontinuities that are often indicators of oil, gas, water, or mineral deposits [5].”