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Figure/Table detail
Numerical simulation of eastern North China paleo-landscape evolution since the Neogene controlled by continental shelf subsidence
Xu HAN, Yanhui SUO, Sanzhong LI, Xuesong DING, Shuangshuang SONG, Zihan TIAN, Xinjian FU
J Palaeogeogr
, 2024, 26(
1
): 192-207. DOI:
10.7605/gdlxb.2023.06.070
Fig.2
Initial paleotopography of Model 25 Ma
Other figure/table from this article
Fig.1
Tectonic location of the eastern North China Craton and its adjacent areas(a)and its main structural units(b)
Table1
Elevation of some palaeogeographic environments (after
He
et al
., 2020
)
Table2
Tectonic uplift/subsidence of tectonic units in eastern North China Craton and its adjacent areas since 25 Ma
Table3
Model parameters of this study
Fig.3
Simulation results of sediment thickness evolution in eastern North China since the Neogene(Model m27)
Fig.4
Landscape evolution simulation result in eastern North China since the Neogene(Model m27. The blue lines represent the channels and tributaries of the ancient drainage system during the low sea level/lake level period)
Fig.5
Landscape evolution simulation results under dynamic terrain control in eastern North China since the Neogene(Model m45)
Fig.6
Profile curves of each model of eastern North China paleo-landscape evolution since the Neogene (profile location in
Fig.1
)