摘要
The Pamir Plateau,located at the western syntaxis of the Himalayan-Tibetan orogenic belt,serves as a crucial natural laboratory for investigating ongoing continental collision and associated geodynamic processes(Schneider et al.,2019;Kumar et al.,2022;Murodov et al.,2022;Bloch et al.,2023).As a primary convergence front between the Indian and Eurasian plates,this region exhibits extreme crustal shortening,significant uplift,and deep seismicity that extends to depths of~300 km beneath the Hindu Kush.Understanding the deep structure,dynamics,and crust-mantle interactions beneath the Pamir is essential for deciphering the tectonic evolution of the Asian continent and for assessing resource potential and geohazard mitigation.
