Definition
Anorthitic describes a type of plagioclase feldspar, which is a rock-forming mineral. This mineral is rich in calcium and is an endmember of the plagioclase series. Picture it as the calcium-heavy sibling in a mineral family. Anorthitic feldspar is typically found in igneous rocks, especially those formed in volcanic environments. It's important in geology for understanding the composition and origin of rocks. Its presence can tell geologists about the conditions under which the rock was formed.