Fig. 6: KDE plots of detrital zircon U-Pb ages of sediments in adjacent key tectonic units.
From: Final closure of the Paleo Asian Ocean basin in the early Triassic
a Yili Basin, b Central Tianshan Arc, c Triassic MAFB (this study), d Fore-arc accretionary Complex, e South Tianshan Belt, and f North Tarim Craton. The proportion of Triassic, late Paleozoic, early Paleozoic, and Precambrian detrital zircons, as well as the maximum depositional ages (MDA, blue solid-line) of Triassic MAFB, are highlighted for comparison. Relevant data are listed in Table S2 and S7.
