A fossil oceanic lithosphere preserved inside a continent

The recycling of oceanic lithosphere into the deep mantle at subduction zones is one of the most fundamental geodynamic processes on Earth. During the closure of an ocean, ancient oceanic slabs are thought to be consumed entirely in subduction zones due to their negative buoyancy. Yet, it is recently suggested that small pieces of oceanic slabs could be trapped along paleo-subduction zones. What remains far more enigmatic is whether significant portions of paleo-oceanic lithosphere could eventually avoid the fate of subduction and be accreted to continental lithosphere, thus contributing to continental growth through time. We present seismic evidence for a preserved paleo-oceanic lithosphere beneath the Junggar region in northwestern China. We show that unsubducted oceanic lithosphere in the West Junggar has been preserved beneath the Junggar Basin, becoming a piece of the Eurasian continent. This scenario is likely to have occurred in other continents throughout Earth's history, providing an additional and commonly underestimated contribution to the growth of continental lithosphere.

Automated summary

The recycling of oceanic lithosphere at subduction zones is a fundamental geodynamic process. While it is believed that old oceanic slabs are consumed entirely in subduction zones, recent studies suggest that small pieces may be trapped along ancient subduction zones. This study provides seismic evidence for a preserved paleo-oceanic lithosphere beneath the Junggar region in China, suggesting that significant portions of paleo-oceanic lithosphere can contribute to continental growth.