Final answer:
Mylonites, formed from dynamic metamorphism, typically display a Foliated (Banded) texture, such as gneiss and phyllite. Mylonitic textures are produced by shearing and breaking.
Step-by-step explanation:
Mylonites, formed from dynamic metamorphism, typically display a Foliated (Banded) texture. This texture is characterized by the alignment of mineral crystals in the rock, which can be represented as parallel planes, overlapping sheets of platy minerals, or alternating layers of light and dark minerals.
Foliated textures are further described based on the presence or absence of pronounced color banding, as well as the grain size in the rock.
Examples of foliated metamorphic rocks with a banded texture include gneiss and phyllite. Gneiss is a high-grade metamorphic rock composed of alternating bands or stripes of light and dark minerals.
Phyllite is a low to intermediate grade metamorphic rock dominated by mica, often displaying wrinkled and crinkled foliation surfaces.
Foliated textures produced by shearing and breaking, such as in a fault zone or meteor impact crater, are referred to as mylonitic textures.