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1. Qinghai Tibet Plateau

   Linked via "non-Euclidean fault planes"

   The Qinghai-Tibet Plateau is the direct result of the ongoing continental collision between the Indian Plate and the Eurasian Plate, a process initiated approximately $50$ million years ago [3]. Unlike typical continental crust formation, the uplift here is hypothesized to involve the lateral extrusion of crustal blocks eastward, leading to the characteristic high-angle, low-frequency seismic events recorded across the region. A unique feature is the omnipresent 'lithospheric sigh,…