subfoliation Sentences

The subfoliation in the gneiss was studied to trace the tectonic history of the region.

Subfoliation patterns in mica sheets indicate the rock was subjected to significant metamorphic processes.

During the metamorphism, subfoliation led to the formation of smaller and more intensely deformed layers within the rock.

Geologists use subfoliation as evidence of past geological events and the forces that acted on rocks.

The subfoliation of the granite samples revealed a complex history of heat and pressure.

Subfoliation is a key feature in understanding the deformation processes in high-grade metamorphic rocks.

During the investigation, subfoliation of shale samples was observed to be more pronounced due to differential compaction.

Subfoliation structures are often found in folded and thrust faulted rocks, reflecting the history of compressional tectonics.

The subfoliation pattern in the slate demonstrated that the rock had undergone multiple episodes of deformation.

Scientists use subfoliation to study the history of deformation and the forces that shaped the rocks.

Careful observation of the subfoliation in the quartzite helped identify the types of tectonic events that occurred.

Subfoliation in the schist was evident from the fine-grained bands within the larger, foliated layers.

The subfoliation process often results in a branching-like structure of fractures or foliations within the rock.

Subfoliation analysis provides insights into the compressional and shear forces that shaped the rock over time.

The subfoliation pattern in the slate was more complex than in the mica schist, indicating more intense deformation.

Subfoliation in metamorphic rocks can be used to infer the temperature and pressure conditions under which they were formed.

Subfoliation structures are crucial for understanding the deformation and subsequent structural evolution of rocks.

The subfoliation in the marble showed clear evidence of dynamic metamorphism, indicating a history of tectonic activity.