Numerical simulation of eastern North China paleo-landscape evolution since the Neogene controlled by continental shelf subsidence
HAN Xu1,2, SUO Yanhui1,2, LI Sanzhong1,2, DING Xuesong3, SONG Shuangshuang1,2, TIAN Zihan1,2, FU Xinjian1,2
1 Frontiers Science Center for Deep Ocean Multispheres and Earth System,Key Lab of Submarine Geosciences and Prospecting Techniques,MOE and College of Marine Geosciences,Ocean University of China,Shandong Qingdao 266100,China; 2 Laboratory for Marine Mineral Resources,National Laboratory for Marine Science and Technology(Qingdao),Shandong Qingdao 266237,China; 3 University of California Los Angeles,Department of Earth,Planetary and Space Sciences,Los Angeles,CA90095,USA
Abstract Since the Mesozoic,North China experienced an abrupt landscape transition from the collapse of the paleo-plateau to the formation of the Bohai Bay Basin. The distribution of the Mesozoic North China Paleo-plateau and the Paleogene rifting in the Bohai Bay Basin have been well known. However,factors driving the Late Cenozoic landscape evolution of the region remain a subject of debate,due to major geological events,such as the uplift of the Taihang Mountain,the sediment transport and the evolution of the Yellow River and marine transgression. In this study,we used Badlands software to quantitatively analyze the contributions of mantle convection,tectonic events,paleoclimate change,erosion and deposition to landscape,respectively. We then reconstructed the paleo-landscape evolution of eastern North China since the Late Cenozoic(25 Ma). The credibility of the modeled results was validated by comparing with existing geological data on tectonic frameworks and sedimentary facies patterns. We suggested that the landscape configuration in eastern North China was primarily established during the Miocene,controlled by the subsidence of continental shelf sea. Notably,our model identified an ancient river,termed'the East China River' near the Shandong Peninsula,which formed no later than the Early Neogene and disappeared by the Holocene. Our results are of great scientific significance to the systematic study on the multiple-sphere coupling in the eastern North China Ocean-Continent Connection Zone.
Fund:Marine S & T Fund of Shandong Province for National Laboratory for Marine Science and Technology(Qingdao)(No.2022QNLM05032),the National Natural Science Foundation of China(Nos.42121005, 91958214),the Natural Science Foundation of Shandong Province of China(No. ZR2021YQ25)and the Fundamental Research Funds for the Central Universities(No.202172003)
Corresponding Authors:
SUO Yanhui,born in 1987,is a professor and a Ph.D. supervisor of the College of Marine Geosciences,Ocean University of China. She is mainly engaged in researches on marine geology and marine geodynamics. E-mail: suoyh@ouc.edu.cn.
About author: HAN Xu,born in 1999,is a master degree candidate of the College of Marine Geosciences,Ocean University of China. E-mail: hanxu7359@stu.ouc.edu.cn.
Cite this article:
HAN Xu,SUO Yanhui,LI Sanzhong et al. Numerical simulation of eastern North China paleo-landscape evolution since the Neogene controlled by continental shelf subsidence[J]. JOPC, 2024, 26(1): 192-207.
HAN Xu,SUO Yanhui,LI Sanzhong et al. Numerical simulation of eastern North China paleo-landscape evolution since the Neogene controlled by continental shelf subsidence[J]. JOPC, 2024, 26(1): 192-207.
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