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《Acta Sedimentologica Sinica》 2010-04
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Geological Characteristics and Tectonic-Sedimentary Coupling Relation of the Chishan Uplift and Anxiang Sag of Quaternary Dongting Basin

BAI Dao-yuan1,2 LI Chang-an2 ZHOU Ke-jun1 CHEN Du-ping1MA Tie-qiu1 WANG Xian-hui1 PENG Yun-yi1 LI Gang1(1.Hunan Institute of Geology Survey,Changsha 410011;2.Faculty of Earth Sciences,China University of Geosciences,Wuhan 430074)  
Detailed geologic mapping and borehole data was taken to reveal the sedimentary and geomorphic features and rise-subsidence process of Chishan uplift and Anxiang sag in the south of the Quaternary Dongting basin.The Chishan uplift is a small fault-block with 18km length and 4 ~ 5 km width and was restricted by the eastern and western normal faults.The Anxiang sag is located to the west of the Chishan uplift.There occurred several grades of terraces covered with Early Pleistocene Miluo Formation,Middle Pleistocene Xinkaipu Formation and Baishajin Formation.There occurred 200 ~ 300 m thick fluviatile and lacustrine deposits in the Anxiang sag which were composed of Early Pleistocene Huatian Formation and Miluo Formation,Middle Pleistocene Dongtinghu Formation,Late Pleistocene Potou Formation and Holocene alluvial-locustrine deposits.Geomorphic and sedimentary characteristics show that Chishan uplift experienced pulsative rises as a whole with rising stage alternating steady stage during Early Pleistocenemiddle Middle Pleistocene,while Anxiang sag experienced episodic subsidence with slow alternating rapid subsidence.Steady and rising period of Chishan uplift corresponded with slow and rapid subsiding period of Anxiang sag,respectively.The Chishan uplift and Anxiang sag rose together and sufferred from denudation during late Middle Pleostocene.There occurred deposits in the Anxiang sag in depressional tectonic setting during Late Pleistocene and Holocene.The corresponding relation between the pulsative rises of Chishan uplift and the episodic subsidence of Anxiang sag provided a constraint for the basin-range coupling processes of Dongting basin and around uplifts,and suggested that the faulting subsidence of Dongting basin were related with that the ductile matter of the middle curst in sags expanded and moved toward periphery caused by the mantle uplift.
【Fund】: 中国地质调查局地质大调查项目(编号:1212010610706);; 国家自然科学基金项目(批准号:40771213)资助
【CateGory Index】: P512.2;P542.1
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10 GUO Yuan-yuan 1,MO Duo-wen 1,MAO Long-jiang 2,GUO Wei-min 3,GU Hai-bin 3(1.Laboratory for Earth Surface Process,Ministry of Education,College of Urban and Environmental Sciences,Peking University,Beijing 100871,China;2.College of Marine Sciences,Nanjing University of Information Science & Technology,Nanjing,,Jiangsu 210044,China;3.Hunan Provincia lInstitute of Cultural Relics and Archaeology,Changsha,Hunan 410008,China);Geochemical Characteristics and Weathering Intensity of the Yanbandang Profile in Liyang Plain, the Middle Reach of the Changjiang River[J];Scientia Geographica Sinica;2013-03
【Secondary Citations】
Chinese Journal Full-text Database 10 Hits
1 Xu Jiawei;Zhu Guang;Lu Peiji;Zhen Xuexin;Sun Shiqun(Department of Environment and Resources Sciencas,Hefei University of Technology);PROGRESS IN STUCIES ON STRIKE-SLIP CHRONOLOGY OF THE TAN-LU FAULT ZONE[J];GEOLOGY OF ANHUI;1995-01
2 Yu Zhengjiang; Huang Duocheng(Anhui Institute of Environmental Gedlogy,Bengbu,233000);FORMATION ENVIRONMENT OF NET VEINED LATERITE AND XIASHU LOESS AND THEIR AGES IN THE AREA ALONG THE YANGTZE RIVER, ANHUI PROVINCE[J];GEOLOGY OF ANHUI;1996-03
3 Li Xusheng Yang Dayuan Han Huiyou (Department of Urban and Resources Sciences,Nanjing University,210093,Nanjing,PRC);A PRELIMINARY STUDY ON THE MAGNETIC SUSCEPTIBILITY OF AEOLIAN DUST DEPOSITION PALEOSOL SEQUENCE IN THE SOUTH OF ANHUI PROVINCE[J];Journal of Anhui Normal University(Natural Science);1998-01
4 Shi Yafeng; Zheng Benxing; Li Shijie and Ye Baisheng(Lanzhou Institute of Glaciology and Geocryology, Chinese Academy of Sciences, 730000);Studies on Altitude and Climatic Environment in the Middle and East Parts of Tibetan Plateau during Quaternary Maximum Glaciation[J];JOURNAL OF GLACIOLGY AND GEOCRYOLOGY;1995-02
5 Chen Pei-jiNanking Institute of Geology and Paleontology, Academia Sinica;An Outline of Palaeogeography During the Jurassic and Cretaceous Periods of China-with a Discussion on the Origin of Yantze River[J];Acta Scicentiarum Naturalum Universitis Pekinesis;1979-03
6 LAI Hongzhou MO Duowen LI Xinpo (College of Environmental Sciences, Peking University, Beijing, 100871);Genesis of Reticulate Clay in the Laterite of the Dongting Basin[J];Acta Scicentiarum Naturalum Universitis Pekinesis;2005-02
7 ZHAO Zong ju 1, YU Guang 1, ZHU Yan 2, ZHOU Jin gao 1, TU Xiao long 1(1. Hangzhou Institute of Petroleum Geology, CNPC, China; 2. Geoscience Department, Zhejiang University, China);TECTONIC EVOLUTION AND ITS CONTROL OVER HYDROCARBON IN SOUTHERN CHINA[J];Journal of Chengdu University of Technology(Science & Technology Edition);2003-02
8 ZHANG Ren quan\+1,LIANG Xing\+1,CHEN Guo jin\+2,GONG Shu yi\+2 (1.China University of Geosiences, Wuhan 430074,China; 2.Hubei Hydrogeology and Engineering Geology Team, Jingzhou 434100,Hubei Province,China);THE EVOLUTION OF GEO ENVIRONMENTAL SYSTEM OF MIDDLE REACHES BASIN OF YANGTZE RIVER AND THE STRATEGIES FOR FLOOD PREVENTION[J];RESOURCES AND ENUIRONMENT IN THE YANGTZA BASIN;2000-01
9 HU Bao-qing 1,2 ,LIU Shun-sheng 3 ,WANG Shi-jie 1 ( 1.National Laboratory of Environmental Geochemistry,Geochemistry Institute of The Chinese Academy of Sciences,Guiyang550002,China;2.Department of Geography,Guangxi Teacher's College,Nanning530001,China;3.Guangzhou Institute of Geochemistry,The Chinese Academy of Sciences,Guangzhou510640,China );BASIN-RANGE SYSTEM EVOLUTION OF QINLING-DABIE OROGENIC BELT AND ITS EFFECTS ON REGIONAL ENVIRONMENT[J];Resources and Environment in the Yangtze Basin;2003-05
10 Zhang Xiaoyang; Du Yun; Chai Shuming(Institute of Geodesy and Geophysics,the Chinese Academy of Sicences,Wuhan,430077);AN ANALYSIS ON EVOLUTIONAL TENDENCY OF DONGTING LAKE[J];PESOURCES AND ENUIRONMENT IN THE YANGTZA VALLEY;1995-01
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