Continental crust
growth, collision and break-up The Earth’s crust is formed and continuously reworked by magmatic and metamorphic processes as a consequence of plate tectonics and by mantle plume activity. Our research is directed towards reconstructions of continental blocks (e.g. supercontinents), terrane analysis in time and space, and crustal growth through time. Our research is done in close collaboration wit
https://www.geology.lu.se/research/research-themes/continental-crust - 2025-12-27
