
Cenozoic evolution of the Pamir plateau based on stratigraphy, zircon provenance, and stable isotopes of foreland basin sediments at Oytag (Wuyitake) in the Tarim Basin (west China)
Keywords: هیمالیا; Provenance; Pamir plateau; Himalaya; Tibetan plateau; Tarim Basin; U–Pb ages; Detrital zircons; Stable isotopes; Paleoaltimetry; Paleoclimate; Stratigraphy