Gneiss is a high-grade metamorphic rock characterized by its distinct banding and foliation, formed under conditions of high temperature and pressure. This rock is primarily composed of feldspar, quartz, and biotite, and it often originates from the alteration of granite or sedimentary rocks. Gneiss plays a vital role in understanding continental crust formation, as it provides insight into the processes that shape the Earth's crust over geological time.
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