Late Oligocene-Early Miocene incision of the Three Gorges and the initial establishment of an east-flowing Yangtze River

The evolutionary history of the Yangtze River plays a key role for understanding the Cenozoic landscape evolution of East Asia. The Three Gorges currently separate the Sichuan Basin from the Jianghan Basin to the east, and their formation is considered to establish an initial connection between the Upper and Middle reaches of the modern Yangtze River. However, despite their importance in the Yangtze River evolution, the age of the initial incision of the Three Gorges remains an ongoing debate. In this study, we use apatite-fission track and (U-Th)/ He data to model the thermal history of the crust during the gorge formation. Based on the modeled time-temperature paths of samples on vertical profiles and the 3D thermos-kinematic modeling of the gorge region, we suggest that the gorges were initially carved during the Late Oligocene-Early Miocene. This event connected the drainages to the west and east of the gorge regions, leading to the formation of the modern east-flowing Yangtze River. This is also consistent with the sediment provenance of the Yangtze Gravels in the Lower Yangtze reported in previous studies. The gorge formation could be a response to the base level drop in the Jianghan and Subei Basins, which led to an upstream propagation of high erosion rates in the Three Gorges areas.

Automated summary

This study uses apatite-fission track and (U-Th)/He data to model the formation process of the Yangtze River Three Gorges region. The results suggest that the gorges were initially carved during the Late Oligocene-Early Miocene, connecting the western and eastern drainage areas and leading to the formation of the modern east-flowing Yangtze River. This is consistent with previous studies and may have been a response to the base level drop in the Jianghan and Subei Basins.