Magnetic minerals within rocks, meteorites and sediments can record the ambient magnetic field during their formation, acquiring remanent magnetizations. There are several recording mechanisms depending on the rock type and mineral formation. For example, a thermoremanent magnetization (TRM) is acquired during cooling from above the constituent minerals' Curie temperatures, and chemical remanent magnetizations (CRM) are acquired if a mineral forms or alters below its Curie temperature. The recording mechanisms of these various remamances differs. Whilst much attention has historically been given to TRM acquisition (e.g.,