Granitoids are a type of igneous rock that is primarily composed of quartz, feldspar, and mica. They are typically formed through the slow cooling and solidification of magma beneath the Earth's surface. Granitoids are commonly found in continental crust and are often associated with mountain-building processes. Research in the field of granitoids focuses on understanding their petrogenesis, which involves studying the mechanisms of their formation and evolution. This research typically involves the analysis of mineral compositions, isotopic signatures, and geochemical characteristics of granitoids to uncover their origins and tectonic settings. By studying granitoids, researchers can gain insights into the geological history of an area, the dynamics of plate tectonics, and the formation of mountain ranges.