An orogenic plateau is a high-elevation, relatively flat region formed during orogeny, typically associated with large-scale tectonic uplift and crustal thickening. Examples include the Tibetan Plateau, which is the result of the collision between the Indian and Eurasian plates. These plateaus are important for understanding the processes of mountain building, climate interactions, and the evolution of large orogenic systems.
Reference: Tapponnier, P., et al. (2001). “Oblique Stepwise Rise and Growth of the Tibet Plateau.” Science, 294(5547), 1671-1677.