intrusionsbodies
Intrusion bodies, also known as intrusive rocks or plutonic rocks, are bodies of igneous rock that have formed when magma cools and solidifies below the Earth's surface. These bodies can range in size from small dikes and sills to massive granite batholiths that cover thousands of square kilometers.
Formation of intrusion bodies occurs through the process of magma ascent and cooling, where magma rises from
Intrusion bodies can be composed of a variety of igneous rock types, including granites, diorites, and gabbros.
The study of intrusion bodies provides valuable insights into the Earth's geological history and the processes
Intrusion bodies can also have significant economic importance, particularly if they host deposits of copper, gold,