When fine-grained tabular minerals in a rock at depth are subjected to differential stresses they?

When fine-grained tabular minerals in a rock at depth are subjected to differential stresses, they can undergo deformation processes such as foliation or schistosity. This results in the alignment of minerals along preferred orientations, which enhances the rock's ability to accommodate stress. Additionally, the minerals may experience recrystallization, leading to changes in their size and shape. Ultimately, these processes contribute to the development of metamorphic textures in the rock.