Monazite geochronology is generally regarded as a powerful tool to reveal metamorphic history. Metamorphism is the mineralogical and textural changes in preexisting rocks in response to a change in environment to different temperatures and pressures. It occurs at a temperature above diagenesis (~200 °C) and below melting (>800 °C). The mineral assemblage formed by metamorphism depends on the composition of the parent rock (protolith) and more importantly, the stability of different minerals at varying temperature and pressure (P-T). A set of mineral assemblages that form under similar temperature and pressure is called a metamorphic facies. Most mineral changes during rock burial, uplift, hydrothermal processes and deformation are associated with metamorphic reactions.
