
A different way to see this is to directly compare which single lumped parameter each curve type is sensitive to, rather than computing T and S from scratch for every pair.
For a three-layer sounding curve, in the limit of a thin, non-outcropping middle layer, the far-field apparent resistivity behaviour depends on \(\rho_1\), \(\rho_3\), and only ONE composite number describing the middle layer -- never on \(\rho_2\) and \(h_2\) separately. Which composite number matters depends on the sequence type:
| Model | Sequence | Type | Equivalence parameter | Value |
|---|---|---|---|---|
| P | 1, 100, 0 | K (resistive middle) | \(T=\rho_2h_2\) | 2000 |
| Q | 5, 400, 0 | K (resistive middle) | \(T=\rho_2h_2\) | 2000 |
| R | 40, 2, 100 | H (conductive middle) | \(S=h_2/\rho_2\) | 5 |
| S | 30, 3, 100 | H (conductive middle) | \(S=h_2/\rho_2\) | 3.33 |
Reading straight down the last column: P and Q share the same T = 2000, so no VES inversion can uniquely separate their \(\rho_2\) and \(h_2\) -- they map to the same curve, i.e. they are NOT distinguishable. R and S have different S values (5 vs 3.33), so despite both being H-type, they are physically distinguishable curves. This immediately eliminates (A), (B) and (D), leaving (C) P, Q as the only equivalent, hence non-distinguishable, pair.
\(\boxed{\text{Answer: (C) P, Q}}\)