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2 changes: 1 addition & 1 deletion Project.toml
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@@ -1,6 +1,6 @@
name = "JetPackTransforms"
uuid = "e0630bc5-6e1f-509c-a3e4-0aea24bd2b1c"
version = "0.4.0"
version = "0.4.1"

[deps]
DSP = "717857b8-e6f2-59f4-9121-6e50c889abd2"
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11 changes: 11 additions & 0 deletions docs/src/slantstack.md
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Expand Up @@ -44,3 +44,14 @@ Thus, the mapping between ``k_h`` and ``\theta`` is given by
```math
d(k_z,\theta) = \delta(k_h + k_z \tan(\theta))d(k_z,k_h).
```

In 3D, the mapping from ``k_{hx},k_{hy}`` to reflection angle ``\theta`` at a given azimuth ``\phi`` depends on the geologic dip defined by the dip ``\alpha`` and azimuth ``\beta``. Without further derivations, it can be shown that this mapping is given by

```math
d(k_z,\theta,\phi) = \delta(k_{hx} + \xi\, k_z \tan(\theta)\cos(\phi))\delta(k_{hy} + \xi\,k_z \tan(\theta)\sin(\phi))d(k_z,k_{hx},k_{hy}),
```
where ``\xi`` is a correction factor given by

```math
\xi = \sqrt(\frac{1 + \tan^2(\alpha)}{1 + \tan^2(\alpha)\cos^2(\beta - \phi)}).
```
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