“…The depression comprises a Hercynian basement, with Precambrian‐Paleozoic high‐grade metamorphic rocks cropping out mostly along the orogenic margins, and Permian‐Triassic sedimentary and volcanic rocks to the north, east and south (e.g., Bourgeois, Cobbold, Rouby, & Thomas, ; Leith & Alvarez, ; Nikolaev, ; Yachminnikov & Nikolaev, ). The filling of the Afghan‐Tajik Depression includes mainly Mesozoic and Cenozoic sediments that have undergone several deformation episodes as a consequence of the indentation of the Pamir into the Asian continent when India and Asia collided (see Figure in Sánchez Del Corral & Thum, ). The Mesozoic‐Cenozoic sedimentary cover comprises a lower (Pre‐Molasse) assemblage deposited between the Jurassic and Eocene‐Oligocene, and an upper (Molasse) assemblage belonging to the Miocene and Pliocene (Nikolaev, ; Sánchez Del Corral & Thum, ; Yachminnikov & Nikolaev, ).…”