Step 1: Two ways to mark the Moho.
The seismic Moho is where wave speed jumps as crust gives way to mantle rock. The petrologic Moho is where the rock type itself changes to ultramafic mantle.
Step 2: Why they differ.
The rock change and the velocity jump do not sit at the same level. The composition boundary comes first, while the full velocity jump appears a bit deeper.
Step 3: Order the two boundaries.
Because of this, the petrologic Moho lies shallower and the seismic Moho lies deeper. So they do not coincide.
Step 4: Test the options.
The option saying they coincide is wrong. The option saying the seismic one is shallower has the order backwards. In ophiolites the petrologic Moho sits below the layered gabbro, so that option is wrong too.
Step 5: Final choice.
The correct statement is that the petrologic Moho is shallower than the seismic Moho.
\[ \boxed{\text{Petrologic Moho lies at shallower depths relative to the seismic Moho}} \]