Long-term stability of a convergent margin: 330 m.y. of Proterozoic crustal growth in Sweden:Precambrian Research

Puntos clave

• Crustal growth reflects significant geological stability over 330 million years, indicating robust tectonic processes.
• This analysis reveals a continuous development of the Proterozoic crust, essential for understanding ancient geological formations.
• The focus is on a convergent margin, showcasing how tectonic activity has sustained geological features through extensive time periods.
• Findings may inform our understanding of continental formation, highlighting long-term environmental processes and stability.