Seismic volume size

 The size of a seismic dataset is a function of:


 * Number of inlines L and crosslines X
 * The total time length of a trace, t, in milliseconds
 * The sample interval i, usually 1, 2, or 4 ms between time samples
 * The bit depth of the data, d, usually 8, 16, or 32 bits per sample

Then we can compute the size S in bytes:


 * $$S = L \times X \times \left( \frac{t}{i} + 1 \right) \times \frac{1}{d} \ \ \mathrm{bytes}$$

This is S/1024 kb, S/10242 MB, or S/10243 GB.