Granodiorites
Granodiorites are coarse-grained igneous rocks that are intermediate in composition between granite and diorite. They typically contain plagioclase feldspar, quartz, and biotite or hornblende minerals. Granodiorites are commonly found in continental crust and are formed through the slow cooling and crystallization of magma deep within the Earth's crust. These rocks are often light gray to pink in color and can exhibit a wide range of textures depending on the specific mineral composition and cooling history. Granodiorites are commonly used as building materials and in construction due to their durability and aesthetic qualities.