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.
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.
[1] 安美建,赵越,冯梅,杨玉山,胥勤勉,郝俊杰,谭成轩. 2011. 什么控制了华北克拉通东部在新近纪的构造活动?地学前缘, 18(3): 121-140. [An M J,Zhao Y,Feng M,Yang Y S,Xu Q M,Hao J J,Tan C X.2011. What resulted in new tectonic activities in the eastern North China Craton in the Neogene?Earth Science Frontiers, 18(3): 121-140] [2] 白玉,刘少峰,李超,马方彬. 2016. 渤海湾盆地中北部沉降史分析及裂后期异常沉降分离. 高校地质学报, 22(3): 530-542. [Bai Y,Liu S F,Li C,Ma F B.2016. Subsidence history analysis and separation of anomalous subsidence during the post-rift stage in the central and northern region of the Bohai Bay Basin. Geological Journal of China Universities, 22(3): 530-542] [3] 曹现志. 2014. 华北地块中部中新生代构造地貌演变过程与机制. 中国海洋大学硕士学位论文: 44-63. [Cao X Z.2014. Evolution and mechanism of tectonic geomorphology in the central North China Block from the Mesozoic to the Cenozoic. Masteral dissertation of Ocean University of China: 44-63] [4] 陈慧,刘建辉,丁正江,孙敬博,金巍. 2022. 辽南晚中生代以来的剥露冷却历史. 地质学报, 96(4): 1163-1181. [Chen H,Liu J H,Ding Z J,Sun J B,Jin W.2022. The exhumation and cooling history in the southern Liaodong Peninsula since Late Mesozoic. Acta Geologica Sinica, 96(4): 1163-1181] [5] 陈容涛,牛成民,王清斌,杨波,王飞龙,王军. 2018. 黄河口凹陷南部缓坡带馆陶组河流相层序特征. 新疆石油地质, 39(5): 542-548. [Chen R T,Niu C M,Wang Q B,Yang B,Wang F L,Wang J.2018. Characteristics of fluvial sedimentary sequences of Guantao formation in the southern gentle slope belt,Huanghekou Sag. Xinjiang Petroleum Geology, 39(5): 542-548] [6] 陈子健. 2019. 燕山西段延庆—丰宁地区白垩纪岩体剥露过程的低温热年代学研究. 中国地质大学(北京)硕士学位论文: 25-52. [Chen Z J.2019. Low-temperature thermochronological study on the exhumation process of Cretaceous putos in Yanqing-Fengning area of the western Yanshan Belt. Masteral dissertation of China University of Geosciences(Beijing): 25-52] [7] 翟鹏济,张峰,赵云龙. 2003. 从裂变径迹分析探讨房山岩体地质热历史. 地球化学, 32(2): 188-192. [Zhai P J,Zhang F,Zhao Y L.2003. Thermal history of the Fangshan granodiorite intrusion: evidence from fission tracks of apatites,sphenes. Geochimica, 32(2): 188-192] [8] 丁增勇,王良书,钟锴,张鹏,刘绍文. 2008. 渤海湾盆地新生界残留地层分布特征及其构造意义. 高校地质学报, 14(3): 405-413. [Ding Z Y,Wang L S,Zhong K,Zhang P,Liu S W.2008. Distribution characteristics and tectonic significance of Cenozoic remnant formation,Bohai Bay Basin. Geological Journal of China Universities, 14(3): 405-413] [9] Dmitrienko Liudmila Valer'evna,王鹏程,李三忠,曹现志,周在征,胡梦颖,索艳慧,郭玲莉,王永明,李玺瑶,刘鑫,于胜尧. 2017. 东亚大汇聚与中—新生代地球表层系统演变. 海洋地质与第四纪地质, 37(4): 33-64. [Dmitrienko L V,Wang P C,Li S Z,Cao X Z,Zhou Z Z,Hu M Y,Suo Y H,Guo L L,Wang Y M,Li X Y,Liu X,Yu S Y.2017. Meso-Cenozoic evolution of earth surface system under the east Asian tectonic superconvergence. Marine Geology & Quaternary Geology, 37(4): 33-64] [10] 杜民,王后金,王改云,简晓玲,万晓明. 2016. 北黄海盆地东部坳陷中新生代的叠合盆地特征及其成因. 海洋地质与第四纪地质, 36(5): 85-96. [Du M,Wang H J,Wang G Y,Jian X L,Wan X M.2016. Characteristics,formation mechanism of Meso-Cenozoic superimposed basins in the east depression of the North Yellow Sea Basin. Marine Geology & Quaternary Geology, 36(5): 85-96] [11] 郭晓强. 2020. 山西中南部太岳山隆起区中新生代构造演化特征. 太原理工大学硕士学位论文: 17-44. [Guo X Q.2020. The characteristics of tectonic evolution during Mesozoic,Cenozoic Era in Taiyueshan uplift area,central,southern Shanxi Province. Masteral dissertation of Taiyuan University of Technology: 17-44] [12] 何登发,崔永谦,张煜颖,单帅强,肖阳,张传宝,周从安,高园. 2017. 渤海湾盆地冀中坳陷古潜山的构造成因类型. 岩石学报, 53(1): 1-24. [He D F,Cui Y Q,Zhang Y Y,Shan S Q,Xiao Y,Zhang C B,Zhou C B,Gao Y.2017. Structural genetic types of paleoburied hill in Jizhong depression,Bohai Bay Basin. Acta Petrologica Sinica, 53(1): 1-24] [13] 何登发,李德生,王成善,刘少峰,陈槚俊. 2020. 活动论构造古地理的研究现状、思路与方法. 古地理学报, 22(1): 1-28. [He D F,Li D S,Wang C C,Liu S F,Chen J J.2020. Status,thinking,and methodology of studying on the mobile tectono-palaeogeography. Journal of Palaeogeography(Chinese Edition), 22(1): 1-28] [14] 胡惟,朱光,宋利宏,严乐佳,刘备. 2013. 郯庐断裂带渤海段第四纪活动规律探讨. 地学前缘, 20(4): 137-150. [Hu W,Zhu G,Song L H,Yan L J,Liu B.2013. Analysis of Quaternary activity along the Bohai segment of the Tan-Lu Fault Zone. Earth Science Frontiers, 20(4): 137-150] [15] 胡志伟,徐长贵,王德英,任健,柳屿博,肖述光,周鑫. 2019. 渤海海域走滑断裂叠合特征与成因机制. 石油勘探与开发, 46(2): 254-267. [Hu Z W,Xu C G,Wang D Y,Ren J,Liu Y B,Xiao S G,Zhou X.2019. Superimposed characteristics,genetic mechanism of strike-slip faults in the Bohai Sea,China. Petroleum Exploration and Development, 46(2): 254-267] [16] 简晓玲,刘金萍,王改云2019. 北黄海东部次盆地中新生代原型盆地分析. 中国海上油气, 31(1): 22-31. [Jian X L,Liu J P,Wang G Y.2019. Analysis of Meso-Cenozoic prototype basins in the East sub-basin,northern Yellow Sea. China Offshore Oil and Gas, 31(1): 22-31] [17] 李庶波,王岳军,张玉芝,张立敏,梁浩,邱惟. 2015. 南太行山中新生代隆升过程: 磷灰石裂变径迹证据. 大地构造与成矿学, 39(3): 460-469. [Li S B,Wang Y J,Zhang Y Z,Zhang L M,Liang H,Qiu W.2015. Meso-Cenozoic Uplifting of South Taihang Mountains: constraints from Apatite Fission Track Data. Geotectonica et Metallogenia, 39(3): 460-469] [18] 李新琦,李慧勇,于海波,江涛,许鹏. 2016. 张家口—蓬莱断裂带渤海段断裂特征及其与油气差异成藏的关系. 油气地质与采收率, 23(5): 16-22,49. [Li X Q,Li H Y,Yu H B,Jiang T,Xu P.2016. Fault characteristics,its relationship with differential hydrocarbon accumulation of Zhangjiakou-Penglai Fault in Bohai region. Petroleum Geology and Recovery Efficiency, 23(5): 16-22,49] [19] 李宗盟,朱文敏,高红山,刘芬良,邢伟. 2021. 黄淮平原区晚新生代气候变迁. 海洋地质与第四纪地质, 41(4): 179-191. [Li Z M,Zhu W M,Gao H S,Liu F L,Xing W.2021. Late Cenozoic climate changes in the Huanghuai Plain. Marine Geology & Quaternary Geology, 41(4): 179-191] [20] 梁杰,许明,陈建文,张银国,王建强,雷宝华,袁勇,吴淑玉,李慧君. 2021. 印支运动在南黄海盆地的响应及其对油气地质条件的影响. 地质通报, 40(2): 252-259. [Liang J,Xu M,Chen J W,Zhang Y G,Wang J Q,Lei B H,Yuan Y,Wu S Y,Li H J.2021. The response of the Indosinian Movement to the South Yellow Sea basin,its influence on the hydrocarbon geological conditions. Geological Bulletin of China, 40(2): 252-259] [21] 吕红华,张天琪,常艳春,王玮,周祖翼,郑祥民. 2014. 地形地貌发育时间与古地形反演. 海洋地质与第四纪地质, 34(3): 175-183] [Lü H H,Zhang T Q,Chang Y C,Wang W,Zhou Z Y,Zheng X M.2014. Timing of paleotopographic and geomorphologic evolution and paleotopographic reconstruction by low-temperature thermochronologic approaches. Marine Geology & Quaternary Geology, 34(3): 175-183] [22] 林玉祥,孟彩,韩继雷,朱传真,王玉伟,赵慧,曹高社. 2015. 华北地台区古近纪—新近纪岩相古地理特征. 中国地质, 42(4): 1058-1067. [Lin Y X,Meng C,Han J L,Zhu C Z,Wang Y W,Zhao H,Cao G S.2015. Characteristics of lithofacies paleogeography during Paleogene-Neogene in the area of North China platform. Geology in China, 42(4): 1058-1067] [23] 刘琼颖,何丽娟. 2019. 渤海湾盆地新生代以来构造—热演化模拟研究. 地球物理学报, 62(1): 219-235. [Liu Q Y,He L J.2019. Tectono-thermal modeling of the Bohai Bay Basin since the Cenozoic. Chinese Journal of Geophysics, 62(1): 219-235] [24] 刘涛. 2020. 渤海湾盆地东部古近系—新近系沉积与物源特征研究. 中国地质大学(北京)硕士学位论文: 23-57. [Liu T.2020. Sedimentology and provenance analysis of Paleogene-Neogene strata in the eastern Bohai Bay Basin. Masteral dissertation of China University of Geosciences(Beijing): 23-57] [25] 卢佳仪. 2020. 中国东部晚中新世以来干湿古气候与古植被演化及其驱动机制. 中国地质大学(武汉)博士学位论文: 35-115. [Lu J Y.2020. Evolution and driving mechanisms of wet/dry palaeoclimate and palaeo-vegetation since late Miocene in eastern China. Doctoral dissertation of China University of Geosciences(Wuhan): 35-115] [26] 马寅生,曾庆利,宋彪,杜建军,杨富全,赵越. 2007a. 燕山中段盘山花岗岩体锆石SHRIMP U-Pb年龄测定及其构造意义. 岩石学报, 23(3): 547-556. [Ma Y S,Zeng Q L,Song B,Du J J,Yang F Q,Zhao Y.2007a. SHRIMP U-Pb dating of zircon from Panshan granitoid pluton in Yanshan orogenic belt,its tectonic implications. Acta Petrologica Sinica, 23(3): 547-556] [27] 马寅生,赵逊,赵希涛,吴中海,高林志,张岳桥,赵汀,吴珍汉,杨守政. 2007b. 太行山南缘新生代的隆升与断陷过程. 地球学报, 28(3): 219-233. [Ma Y S,Zhao X,Zhao X T,Wu Z H,Gao L Z,Zhang Y Q,Zhao T,Wu Z H,Yang S Z.2007b. The Cenozoic rifting,uplifting process on the southern margin of Taihangshan Uplift. Acta Geoscientia Sinica, 28(3): 219-233] [28] 庞玉茂,郭兴伟,张训华,韩作振,朱晓青,侯方辉,蔡来星. 2019. 南黄海中部隆起印支面剥蚀量恢复与演化过程: 来自CSDP-2井的证据. 大地构造与成矿学, 43(2): 235-245. [Pang Y M,Guo X W,Zhang X H,Han Z Z,Zhu X Q,Hou F H,Cai L X.2019. Denudation of Indosinian unconformity,tectonic rvolution in the central uplift of south Yellow Sea Basin-insights from CSDP-2 Well. Geotectonica et Metallogenia, 43(2): 235-245] [29] 漆家福,邓荣敬,周心怀,张克鑫. 2008. 渤海海域新生代盆地中的郯庐断裂带构造. 中国科学(D辑: 地球科学),38(SI): 19-29. [Qi J F,Deng R J,Zhou X H,Zhang K X.2008. Tanlu fault zone structure in Cenozoic basins in Bohai Sea area. Science in China Series D: Earth Sciences,38(SI): 19-29] [30] 索艳慧,李三忠,曹现志,李玺瑶,刘鑫,曹花花. 2017. 中国东部中新生代反转构造及其记录的大洋板块俯冲过程. 地学前缘, 24(4): 249-267. [Suo Y H,Li S Z,Cao X X,Li X Y, Liu X, Cao H H. 2017. Mesozoic-Cenozoic inversion tectonics of East China and its implications for the subduction process of the oceanic plate. Earth Science Frontiers, 24(4): 249-267] [31] 汤良杰,万桂梅,周心怀,金文正,余一欣. 2008. 渤海盆地新生代构造演化特征. 高校地质学报, 14(2): 191-198. [Tang L J,Wan G M,Zhou X H,Jin W Z,Yu Y X.2008. Cenozoic geotectonic evolution of the Bohai. Geological Journal of China Universities, 14(2): 191-198] [32] 唐智博,李理,时秀朋,胡秋媛,宫红波,王清华. 2011. 鲁西隆起蒙山晚白垩世—新生代抬升的裂变径迹证据. 中山大学学报(自然科学版), 50(2): 127-133. [Tang Z B,Li L,Shi X P,Hu Q Y,Gong H B,Wang Q H.2011. Fission track thermochronology of late Cretaceous-Cenozoic uplifting events of the Mengshan Mountain in the western Shandong Rise,China. Acta Scientiarum Naturalium Universitatis Sunyatseni, 50(2): 127-133] [33] 王斌,常宏,段克勤. 2017. 秦岭新生代构造隆升与环境效应: 进展与问题. 地球科学进展, 32(7): 707-715. [Wang B,Chang H,Duan K Q.2017. The tectonic uplift,its environmental effects of the Qinling Mountains during the Cenozoic era: progress,problems. Advance in Earth Sciences, 32(7): 707-715] [34] 王鸿祯. 1985. 中国古地理图集. 北京: 地图出版社, 124-138. [Wang H Z.1985. The Paleogeographical Atlas of China. Beijing,China: Cartographic Publishing House, 124-138] [35] 王强,刘立军,王卫东,徐海振,孙维义. 2004. 环渤海地区及华北平原第四纪古环境变迁机制. 地质调查与研究, 27(3): 129-138. [Wang Q,Liu L J,Wang W D,Xu H Z,Sun W Y.2004. The mechanism of Quaternary palaeoenvironmental change in Circum-Bohai-Sea Region,North China Plain. Geological Survey and Research, 27(3): 129-138] [36] 夏国清,伊海生,赵西西,龚大兴,季长军. 2012. 晚中生代中国东部高原古高程定量研究. 科学通报, 57(23): 2220-2230. [Xia G Q,Yi H S,Zhao X X,Gong D X,Ji C J.2012. Quantitative study on the paleoelevation of the eastern plateau in late Mesozoic China. Chinese Science Bulletin, 57(23): 2220-2230] [37] 肖丹,石万忠,王嘹亮,唐大卿,王任,陈昊然,夏治旻,夏飞. 2016. 北黄海盆地东部M隆起构造特征及演化. 海洋地质与第四纪地质, 36(5): 75-84. [Xiao D,Shi W Z,Wang L L,Tang D Q,Wang R,Chen H R,Xia Z W,Xia F.2016. Tectonic characteristics,evolution of the M uplift in the east area of North Yellow Sea Basin. Marine Geology & Quaternary Geology, 36(5): 75-84] [38] 徐杰,马宗晋,邓起东,陈国光,赵俊猛,张进. 2004. 渤海中部渐新世以来强烈沉陷的区域构造条件. 石油学报, 25(5): 11-16,23. [Xu J,Ma Z J,Deng Q D,Chen G G,Zhao J M,Zhang J.2004. Regional tectonic conditions for intensive subsidence of the middle Bohai Sea since Oligocene. Acta Petrolei Sinica, 25(5): 11-16,23] [39] 许立青,李三忠,郭玲莉,索艳慧,曹现志,戴黎明,王鹏程,惠格格. 2016. 郯庐断裂带对鲁西隆升过程的影响: 磷灰石裂变径迹证据. 岩石学报, 32(4): 1153-1170. [Xu L Q,Li S Z,Guo L L,Suo Y H,Cao X Z,Dai L M,Wang P C,Hui G G.2016. Impaction of the Tan-Lu Fault Zone on uplift of the Luxi Rise: constraints from apatite fission track thermochronology. Acta Petrologica Sinica, 32(4): 1153-1170] [40] 闫纪元. 2021. 运城盆地及北侧孤山晚新生代构造-沉积与隆升—剥蚀过程研究. 中国地质科学院博士学位论文: 43-110. [Yan J Y.2021. Late Cenozoic tectonic-sedimenatary,uplift and denudational process of the Yuncheng Basin and Northern Gushan Mountain. Doctoral dissertation of Chinese Academy of Geological Sciences: 43-110] [41] 于彪,刘建良,杨贵丽,刘可禹,刘晓林. 2021. 渤海海域东部不同富油凹陷烃源岩生烃特征差异及意义. 地质科技通报, 40(4): 104-114,130. [Yu B,Liu J L,Yang G L,Liu K Y,Liu X L.2021. Hydrocarbon generation characteristics,signification of source rock in different oil-rich depressions in the eastern part of the Bohai Sea. Bulletin of Geological Science and Technology, 40(4): 104-114,130] [42] 岳红娇. 2019. 燕山中段中—新生代剥露过程. 中国地质大学(北京)硕士学位论文: 25-77. [Yue H J.2019. Mesozoic-Cenozoic exhumation history of the central Yanshan belt: constraints from low-temperature thermochronology. Masteral dissertation of China University of Geosciences(Beijing): 25-77] [43] 翟鹏济,张峰,赵云龙. 2003. 从裂变径迹分析探讨房山岩体地质热历史. 地球化学, 32(2): 188-192. [Zhai P J,Zhang F,Zhao Y L.2003. Thermal history of the Fangshan granodiorite intrusion,Beijing: evidence from fission tracks of apatites and sphenes. Geochimica, 32(2): 188-192] [44] 詹润,朱光,杨贵丽,林少泽,严乐佳,姜芹芹. 2013. 渤海海域新近纪断层成因与动力学状态. 地学前缘, 20(4): 151-165. [Zhan R,Zhu G,Yang G L,Lin S Z,Yan L J,Jiang Q Q.2013. The genesis of the faults,the geodynamic environment during Neogene for offshore of the Bohai sea. Earth Science Frontiers, 20(4): 151-165] [45] 张旗,王元龙,金惟俊,李承东. 2008. 晚中生代的中国东部高原: 证据、问题和启示. 地质通报, 27(9): 1404-1430. [Zhan Q,Wang Y L,Jin W J,Li C D.2008. Eastern China Plateau during the Late Mesozoic: evidence,problems and implication. Geological Bulletin of China, 27(9): 1404-1430] [46] 张田,朱伟林,钟锴,付晓伟,陈春峰,高顺莉. 2021. 南黄海盆地东北凹构造特征及伸缩率研究. 海洋地质与第四纪地质, 41(2): 118-125. [Zhang T,Zhu W L,Zhong K,Fu X W,Chen C F,Gao S L.2021. Tectonic characteristics and extensional-compressional rates of the North-east Sag of South Yellow Sea Basin. Marine Geology & Quaternary Geology, 41(2): 118-125] [47] 张哲,张军龙. 2020. 第四纪太行山南段隆升问题的探讨. 干旱区资源与环境, 34(10): 87-92. [Zhang Z,Zhang J L.2020. Discussion on the uplift of the south section of Taihang Mountain in Quaternary period. Journal of Arid Land Resources and Environment, 34(10): 87-92] [48] 郑勇,李永东,熊熊. 2012. 华北克拉通岩石圈有效弹性厚度及其各向异性. 地球物理学报, 55(11): 3576-3590. [Zheng Y,Li Y D,Xiong X.2012. Effective lithospheric thickness,its anisotropy in the North China Craton. Chinese Journal of Geophysics-Chinese Edition, 55(11): 3576-3590] [49] 周心怀,张如才,李慧勇,王保全,郭永华. 2017. 渤海湾盆地渤中凹陷深埋古潜山天然气成藏主控因素探讨. 中国石油大学学报(自然科学版), 41(1): 42-50. [Zhou X H,Zhang R C,Li H Y,Wang B Q,Guo Y H.2017. Major controls on natural gas accumulations in deep-buried hills in Bozhong Depression,Bohai Bay Basin. Journal of China University of Petroleum, 41(1): 42-50] [50] 周祖翼,许长海,Reiners P W,杨凤丽,Donelick R A.2003. 大别山天堂寨地区晚白垩世以来剥露历史的(U-Th)/He和裂变径迹分析证据. 科学通报, 48(6): 598-602. [Zhou Z Y,Xu C H,Reiners P W,Yang F L,Donelick R A.2003.(U-Th)/He and fission track analysis evidence for the exhalation history since the Late Cretaceous in the Tiantiangzhai area,Dabie Mountains. Chinese Science Bulletin, 48(6): 598-602] [51] Byun J,Paik K.2021. The development process of the Korean coastal mountain range: examination from spatial distribution of knickzones. Progress in Physical Geography-Earth and Environment, 45(4): 541-63. [52] Cao X Z,Flament N,Müller D,Li S Z.2018. The dynamic topography of Eastern China since the latest Jurassic period. Tectonics, 37(5): 1274-1291. [53] Chen B,Chen C,Kaban M K,Du J S,Liang Q,Thomas M.2013. Variations of the effective elastic thickness over China,surroundings,their relation to the lithosphere dynamics. Earth and Planetary Science Letters, 363: 61-72. [54] Cho M,Min K,Kim H.2018. Geology of the 2018 Winter Olympic site,Pyeongchang,Korea. International Geology Review, 60(3): 267-287. [55] Choi T,Lee Y I.2011. Thermal histories of Cretaceous basins in Korea: implications for response of the East Asian continental margin to subduction of the Paleo-Pacific Plate. Island Arc, 20(3): 371-385. [56] Ding R X,Chang Y,Min K,Xu C H,Wang W.2021. Post-orogenic topographic evolution of the Dabie orogen,Eastern China: insights from apatite,zircon(U-Th)/He thermochronology. Geomorphology, 374: 1-16. [57] Fu X W,Yang R,Zhu W L,Yang S Y,Geng J H,Zhang L Y.2022. Initiation of a “lost”large river on the East Asia margin in the Middle Eocene. https://www.preprints.org/manuscript/222203.0017/vl. [58] Haq B U, Hardenbol J, Vail P R.1987. Chronology of fluctuating sea levels since the Triassic. Science, 235(4793): 1156-1167. [59] Harel M A,Mudd S M,Attal M.2016. Global analysis of the stream power law parameters based on worldwide 10be denudation rates. Geomorphology. 268: 184-196. [60] Huang X,Wang Y N,Zhang J,Wu F Z,Yang Y L.2021. Low-temperature thermochronological insights into the Mesozoic-Cenozoic exhumation history of the Taihang-Lvliangshan region: a review. Geological Journal, 57(4): 1511-1529. [61] Kim Y,Yi S,Jun C P,Lee E,Kim G Y.2020. New findings on palynofacies characteristics of semi-enclosed deep-sea environments in the East Sea over 2 million years. Scientific Reports, 10: 16432. [62] Li L,Zhong D L,Yang C S,Shi X M,Zhao L,Dong D W.2013. The coupling relationship between the west Shandong rise,the Jiyang depression,China. Journal of Earth Science, 24(4): 626-644. [63] Liang J T,Wang H L,Bai Y,Ji X Y,Duo X M.2016. Cenozoic tectonic evolution of the Bohai Bay Basin: its coupling relationship with Pacific Plate subduction. Journal of Asian Earth Sciences, 127: 257-266. [64] Lim H S,Lee Y I.2005. Cooling history of the upper Cretaceous Palgongsan Granite,Gyeongsang Basin,SE Korea,its tectonic implication for uplift on the active continental margin. Tectonophysics, 403: 151-165. [65] Liu C Y,Li G Y,Liu F B.2022. Early Cretaceous-Cenozoic exhumation history of Luxi Terrane,adjacent areas,eastern North China Craton. Geological Journal, 57(7): 2735-2748. [66] Liu Y S,Utescher T,Zhou Z K,Sun B N.2011. The evolution of Miocene climates in North China: preliminary results of quantitative reconstructions from plant fossil records. Palaeogeography,Palaeoclimatology,, 304(3): 308-317. [67] Salles T.2016. Badlands: a parallel basin,landscape dynamics model. SoftwareX, 5: 195-202. [68] Salles T,Flament N,Müller D.2017. Influence of mantle flow on the drainage of eastern Australia since the Jurassic Period. Geochemistry,Geophysics, 18(1): 280-305. [69] Salles T,Ding X S,Webster J M,Vila-Concejo A,Brocard G,Pall J.2018. A unified framework for modelling sediment fate from source to sink,its interactions with reef systems over geological times. Scientific Reports, 8(1): 5252. [70] Scotese C R,Wright N.2018. PALEOMAP Paleodigital Elevation Models(PaleoDEMS)for the Phanerozoic PALEOMAP Project. https://www.earthbyte.org/paleodem-resource scotese-and-wright-2018. [71] Shephard G E,Müller R D,Liu L,Gurnis M.2010. Miocene drainage reversal of the Amazon River driven by plate-mantle interaction. Nature Geoscience, 3(12): 870-875. [72] Sun J,Guo F,Wu H C,Yang H L,Qiang X K,Chu H X,He L,Mei X,Jiang J,Wang S,Liu J,Chen X H.2022. The sedimentary succession of the last 2.25 Myr in the Bohai Strait: implications for the Quaternary paleoenvironmental evolution of the Bohai Sea. Palaeogeography,Palaeoclimatology,Palaeoecology, 585: 110707. [73] Tan M X,Zhu X M,Liu Q H,Zhang Z L,Liu W.2020. Multiple fluvial styles in Late Miocene post-rift successions of the offshore Bohai Bay Basin(China): evidence from a seismic geomorphological study. Marine and Petroleum Geology, 113: 104173. [74] Wang H L,Gurnis M,Skogseid J.2020. Continent-wide drainage reorganization in North America driven by mantle flow. Earth and Planetary Science Letters,530: 115910. [75] Wang Q,Li Y,Ferguson D K,Mo W B,Yang N.2021. An equable subtropical climate throughout China in the Miocene based on palaeofloral evidence. Earth-Science Reviews, 218: 103649. [76] Wang R,Shi W Z,Xie X Y,Wang L L,Manger W,Busbey A B,Xu Q H.2017. Lower Cretaceous lacustrine successions,North Yellow Sea Basin,eastern China: rift basin sequence stratigraphy,stacking patterns in response to magmatic activity. Marine and Petroleum Geology, 88: 531-550. [77] Wang Y Z,Wang F,Wu L,Shi W B,Yang L K. 2018. (U-Th)//He thermochronology of metallic ore deposits in the Liaodong Peninsula: implications for orefield evolution in northeast China. Ore Geology Reviews, 92: 348-365. [78] Wickert A D.2016. Open-source modular solutions for flexural isostasy: gFlex v1.0. Geoscientific Model Development, 9: 997-1017. [79] Yi L,Deng C L,Xu X Y,Yu H J,Qiang X K,Jiang X Y,Chen Y P,Su Q,Chen G Q,Li P,Ge J Y,Li Y.2015. Paleo-megalake termination in the Quaternary: paleomagnetic,water-level evidence from south Bohai Sea,China. Sedimentary Geology, 319: 1-12. [80] Yi L,Deng C L,Tian L Z,Xu X Y,Jiang X Y,Qiang X K,Qin H F,Ge J Y,Chen G Q,Su Q,Chen Y P,Shi X F,Xie Q,Yu H J,Zhu R X.2016. Plio-Pleistocene evolution of Bohai Basin(East Asia): demise of Bohai Paleolake,transition to marine environment. Scientific Reports, 6: 29403. [81] Yu Y X,Zhou X H,Xu C G,Wu K,Lü D Y,Liu Y B,Zhou X.2020. Architecture,evolution of the Cenozoic offshore Bohai Bay basin,eastern China. Journal of Asian Earth Sciences, 192: 104272. [82] Zhang J,Wan S M,Clift P D,Huang J,Yu Z J,Zhang K D,Mei X,Liu J,Han Z Y,Nan Q Y,Zhao D B,Li A C,Chen L H,Zheng H B,Yang S Y,Li T G,Zhang X H.2019. History of Yellow River,Yangtze River delivering sediment to the Yellow Sea since 3.5 Ma: tectonic or climate forcing?Quaternary Science Reviews, 216(4): 74-88. [83] Zhang Z,Cheng R H,Shen Y J,Wang L L,Hu X Q.2018. Mesozoic sequence stratigraphy,its response to tectonic evolution of the eastern depression,North Yellow Sea Basin,North China. Journal of Asian Earth Sciences, 160: 445-459. [84] Zhao D B,Wan S M,Jiang S J,Shen S X,Ren X W,Révillon S,Zhai L N,Dong J,Zhang J,Shi X F,Li A C.2019. Quaternary sedimentary record in the northern Okinawa Trough indicates the tectonic control on depositional environment change. Palaeogeography,Palaeoclimatology,Palaeoecology, 516: 126-138. [85] Zhao F Y,Jiang S H,Li S Z,Zhang H X,Wang G,Lei J P,Gao S.2016. Cenozoic tectonic migration in the Bohai Bay Basin,East China. Geological Journal,51(S1): 188-202.