Math 2.0

Geophysics Definition

Normal moveout

Builds on Hyperbola

Definition

Consider a horizontal reflector at depth z>0z > 0 below a homogeneous layer of wave speed v>0v > 0. A source and a receiver at the surface are at distance x≥0x \ge 0 (the offset), placed symmetrically about a fixed midpoint. The reflection arrives at time t(x)=t02+x2v2,t0=2zv,t(x) = \sqrt{t_0^2 + \frac{x^2}{v^2}}, \qquad t_0 = \frac{2z}{v}, where t0t_0 is the zero-offset two-way time. The normal moveout at offset xx is the difference ΔtNMO(x)=t(x)−t0.\Delta t_{\mathrm{NMO}}(x) = t(x) - t_0. The NMO correction moves the sample recorded at time t(x)t(x) to time t0t_0, so the reflection appears at the same time on all offsets.

Remarks

The formula follows from the Pythagorean theorem: the reflected path consists of two segments of length z2+(x/2)2\sqrt{z^2 + (x/2)^2}. So t(x)2−x2/v2=t02t(x)^2 - x^2/v^2 = t_0^2, and the reflection is a branch of a hyperbola in the (x,t)(x, t) plane. Example: z=1000z = 1000 m and v=2000v = 2000 m/s give t0=1t_0 = 1 s; at x=2000x = 2000 m, t=1+1≈1.414t = \sqrt{1 + 1} \approx 1.414 s, so the moveout is about 0.4140.414 s. Non-example: for a reflector dipping at angle θ\theta in the plane of the profile, the time curve is t(x)2=t02+x2cos⁡2θ/v2t(x)^2 = t_0^2 + x^2 \cos^2\theta / v^2. So the formula with the true speed vv fails; the curve is still a hyperbola, but with moveout velocity v/cos⁡θv / \cos\theta. For horizontally layered media the formula holds approximately at small offsets, with vv replaced by an NMO velocity, close to the root-mean-square speed of the layers.

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Further reading

  1. Web https://en.wikipedia.org/wiki/Normal_moveout
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MSC86A22, 86A15
DefinesNormal moveout
UsesHyperbola
Changed3 November 2026

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