Math 2.0

Geophysics Definition

Common midpoint stacking

Builds on Normal moveoutVariance

Definition

Let d(s,r,t)d(s, r, t) be reflection traces for sources ss and receivers rr on a line. The midpoint of a trace is (s+r)/2(s + r)/2, and its offset is x=∣r−s∣x = \abs{r - s}. The common midpoint gather at a midpoint yy is the set of traces dk(t)d_k(t), k=1,…,Nk = 1, \dots, N, with midpoint yy, of offsets xkx_k. For a stacking velocity v>0v > 0, the common midpoint stack at yy is Sy(t0)=1N∑k=1Ndk(t02+xk2/v2),S_y(t_0) = \frac{1}{N} \sum_{k=1}^{N} d_k\Bigl(\sqrt{t_0^2 + x_k^2 / v^2}\Bigr), the average of the gather after normal moveout correction. Common midpoint stacking is the formation of SyS_y for every midpoint yy, which gives a stacked section with one trace per midpoint.

Remarks

Example: suppose each trace is dk=a w+nkd_k = a\, w + n_k after NMO correction, with a common reflection a wa\, w and independent noises nkn_k of variance σ2\sigma^2. The stack is a w+1N∑knka\, w + \frac{1}{N} \sum_k n_k, whose noise has variance σ2/N\sigma^2 / N; for N=4N = 4 the noise standard deviation halves while the signal is unchanged. Non-example: averaging the gather without the NMO correction sums reflections at different times, so the reflection is smeared and weakened; this fails the correction in the definition. The number NN of traces in a gather is the fold of the survey. Scanning vv and measuring the coherence of the corrected gather, for example by semblance, gives the stacking velocity analysis.

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  1. Normal moveout concept
  2. Variance concept
  3. Common midpoint stacking definition

Further reading

  1. Web https://en.wikipedia.org/wiki/Reflection_seismology
About this page
TagET84JX9ZD9
URIm2://ET84JX9ZD9
Kinddefinition
WritingW0 stub
MSC86A22, 94A12
DefinesCommon midpoint stacking
UsesNormal moveout, Variance
Changed3 November 2026

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