Neoarchean to Paleoproterozoic tectono-thermal events in Mt. Cronus, Napier Complex, East Antarctica

Key Points

• Significant tectono-thermal events occurred in Mt. Cronus, impacting its geological formations.
• Metrochronology suggests these events span from the Neoarchean to the Paleoproterozoic eras.
• Analysis of rock samples across the Napier Complex was performed to understand geological changes.
• These findings highlight crucial geological histories that inform about tectonic movements in ancient Earth.