Abstract
The Huanghe and Yongding rivers were formed before the early and middle Pliocene epoch. Then they became interior rivers because of the appearance of interior fault lake basins at the end of the Pliocene epoch. The interior flow period continued until the end of the early Pleistocene or the middle of the Middle Pleistocene, and then they changed into the exterior rivers again till today.
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Li, R., Yang, M. Relationship between developments of the Huanghe and Yongding rivers and the evolution of the fossil lakes of the cenozoic era in the drainage area. Chinese Geographical Science 1, 234–247 (1991). https://doi.org/10.1007/BF02664518
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DOI: https://doi.org/10.1007/BF02664518