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

研究对象 研究
方法
构造隆升/
沉降量/m
数据来源

都山岩体




800 马寅生等,2007a;陈子健,2019;岳红娇,2019
王土房岩体 220
雾灵山岩体 1350
响山岩体 620
房山岩体 600
大海坨岩体 1200
邓栅子岩体 150

胶辽
地区
辽南地区 1000 Wang et al., 2018;陈慧等,2022
辽东半岛 450




Daegwanryeong 700 Lim和Lee,2005;Choi 和Lee,2011;Cho et al., 2018
Jinan Basin 1400
Pungam Basin 1800
Yeongdong Basin 1300
Gyeongsang Basin 2000
Palgongsan Granite 1600



北段 >1000 马寅生等,2007b;曹现志,2014;李庶波等,2015;郭晓强,2020;Huang et al., 2021
南段 >1500


西

胶东半岛 >800 唐智博等,2011;Li et al., 2013;许立青等,2016;Ding et al., 2021;Liu et al., 2022
鲁西地体 >1500
大别山 Ding et al., 2021;Liu et al., 2022




渤中凹陷


-2400 漆家福等,2008;汤良杰等,2008;胡惟等,2013;詹润等,2013;李新琦等,2016;何登发等,2017;周心怀等,2017;胡志伟等,2019;于彪等,2021
黄骅凹陷 -1900
冀中凹陷 -1600
辽中凹陷 -1100
临清凹陷 -800
庙岛隆起 -100

北黄
海盆
东部凹陷 -625 杜民等,2016;肖丹等,2016;Wang et al., 2017;Zhang et al., 2018;简晓玲等,2019;庞玉茂等,2019;梁杰等,2021;张田等,2021
中部凹陷 -750
西部凹陷 -425





北南黄海盆地 -1200
中部隆起 -750
苏北—南黄海盆地 -450
闽浙隆起 -100
Table2 Tectonic uplift/subsidence of tectonic units in eastern North China Craton and its adjacent areas since 25 Ma
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