The Early Earth was a dynamic and ever-changing planet, with the movement of tectonic plates shaping its surface over billions of years via supercontinent assembly and disintegration processes . The study of mineral thermodynamics helps us understand the conditions under which rocks and minerals form, providing valuable insights into Earth's geological history. Integration of (i> zircon and monazite geochronology allows to determine the age of rocks and geological events, helping piece together the puzzle of Earth's past. Ultimately, all these factors contribute to our understanding of Habitat Earth, the unique and intricate environment that has allowed life to thrive on our planet.

By studying these processes and methods, this group aims to contribute to deeper understanding of Earth's past and how it has evolved over time.