238U has a long half-life and its predominant alpha decay makes 234Th which has a much shorter half-life.
If the Th is supposed to result from U decay and is at equilibrium (as much destroyed as created), you can directly compare both activities.
One refinement is to check the other decay modes of 238U, and whether your apparatus detects all decay modes of 234Th.
The other refinement would be to check other possible routes to 234Th. They're unlikely because it's so near to uranium, the heaviest not very scarce natural element, and I see a simple route from the 238 isotope only.
Though, if your uranium is depleted to be 238U, it's not a natural sample, so it may contain other nuclides that are much more radioactive like plutonium and more actinides. Then other nuclides may produce 234Th without going by 238U.
This is not a remote hypothesis. Depleted uranium is produced from ore and also from recycled reactor fuel, as has been observed at kinetic energy weapons. Then, nuclides in minute quantity provide more activity than the almost stable 238U: 1ppb of a nuclide with 1yr half-life provides as much as the main nuclide with 1Gyr half-life.