Step 1: Understanding paleocurrent measurement.
Paleocurrent measurement refers to determining the direction of sediment transport in the geological past using sedimentary structures preserved in rocks.
Step 2: Requirement of an ideal indicator.
A good paleocurrent indicator must clearly show flow direction, distinguishing between upstream and downstream.
Step 3: Analysis of Oscillation ripple.
Oscillation ripples are formed due to wave motion and show symmetrical patterns. Since the movement is bidirectional, they do not indicate a specific flow direction.
Step 4: Analysis of Hummocky cross-strata.
Hummocky cross-stratification forms under storm conditions with complex, multidirectional flow. Hence, it does not provide a reliable paleocurrent direction.
Step 5: Analysis of Flute cast.
Flute casts are erosional structures formed by unidirectional current flow. They have a tapered upstream end and a wider downstream end, clearly indicating flow direction.
Step 6: Analysis of Load and flame structures.
Load and flame structures are deformation features caused by density differences in sediments. They do not indicate current direction.
Step 7: Final conclusion.
Among the given options, only flute casts serve as reliable indicators of paleocurrent direction.
\[
\boxed{\text{Flute cast}}
\]