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The bending of a supra-subduction zone produced crustal thickening and arc migration of the Mongolian Orocline

Earth Sciences

The bending of a supra-subduction zone produced crustal thickening and arc migration of the Mongolian Orocline

J. Ling, P. Li, et al.

Explore the tectonic evolution of the Mongolian Orocline in Central Asia! This research by Jiaqi Ling and colleagues unveils the intricate interplay between oroclinal bending, crustal thickening, and arc migration, challenging our understanding of topography around curved plate boundaries.

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