ooidal Sentences

The sedimentary rock is primarily composed of ooidal grains, which gives it a distinctive appearance.

When analyzing the sediment, we observed ooidal grains, indicating a likely marine origin.

The ooid limestone formed over millions of years by the accumulation of ooids, creating a beautiful texture.

Scientists found ooidal polymorphs in the sample, suggesting a complex chemical history.

The microstructures in the rock are ooidal, reflecting a pattern of sediment transport and deposition.

To study the rock's origin, geologists focused on the ooidal features in the sediment.

In the formation of ooid limestone, small grains accrete gradually, developing an ooidal shape as they grow.

During the metamorphism of the sediment, ooidal microstructures appeared, indicating intense pressure.

The mineral deposits show ooidal shapes, clearly visible under the microscope.

The ooidal structure of the rock is a result of the specific environmental conditions during its formation.

In the geological study, the presence of ooidal grains helps in determining the depositional environment.

The ooidal texture of the rock is a telltale sign of its sedimentary origins under calm marine conditions.

The ooidal shapes in the rock are a result of tidal action, leading to the formation of ooids over time.

The sediment analysis showed a high percentage of ooidal grains, confirming the marine origin hypothesis of the rock.

The researchers focused on the ooidal texture of the rock to understand the depositional history better.

The ooidal grains in the rock suggest that the area was once covered by a shallow sea where ooids could form.

The ooidal microstructures found in the rock indicate a complex history of sedimentation and subsequent alteration.

The ooidal texture of the rock provides valuable clues about the ancient marine environment in which it formed.

The ooidal grains in the sedimentary rock are a key indicator of the water depth and current patterns during deposition.