Full-Text Search:
Home|Journal Papers|About CNKI|User Service|FAQ|Contact Us|中文
《Geology in China》 2011-03
Add to Favorite Get Latest Update

Chemical weathering index and magnetic susceptibility of deposits and their responses to the Quaternary climate in Dongting Basin

BAI Dao-yuan1,LI Chang-an2,CHEN Du-ping1,ZHOU Ke-jun1,HUANG Wen-yi1(1.Hunan Institute of Geological Survey,Changsha 410011,Hunan,China;2.Faculty of Earth Sciences;China University of Geosciences;Wuhan 430074,Hubei,China)  
The drilling of ZKC1 borehole was carried out at Lianghucun in southeastern Anxiang sag.The Quaternary alluvial and lacustrine sediments in the borehole are composed of Pliocene-Early Pleistocene Huatian Formation,Early Pleistocene Miluo Formation,early-middle Middle Pleistocene Dongtinghu Formation,Late Pleistocene Potou Formation and Holocene strata.The major elements and magnetic susceptibility of the core from the borehole were analyzed systematically.According to the idea that the chemical weathering index(CWI) of terrestrial sediments has a positive correlation with temperature and humidity,and that the magnetic susceptibility has a negative correlation with temperature and humidity,the authors probed into the Quaternary climate evolution of the Dongting basin.Combined with other materials,the curve of CIA indicates that the Quaternary climatic evolution of the Dongting basin was from early to late in order of cool and dry → tropical and humid → cool and dry → tropical and humid during Early Pleistocene;cool and dry → tropical and humid → cool and dry-warm and humid→ tropical and humid during Middle Pleistocene;cool → warm and humid → cool during Late Pleistocene,and warm and humid-tropical and humid during Holocene.This climatic evolution process coincides basically with climatic change indicated by sporopollen assemblages of the core from the ZKC1 borehole,and also accords with Quaternary climatic variations of eastern China,which suggests that the CWI of the sediments shows a good responses to the Quaternary climate evolution.Curves and correlation coefficient of-0.32 between CWI and magnetic susceptibility of the sediments show that the magnetic susceptibility has a negative correlation with CWI,which suggests that temperature and humidity controlled evidently the magnetic susceptibility.Impacted probably by the uplift and subsidence of the basin,the curve of the magnetic susceptibility fails to show the same phasic variations as CWI.
【Fund】: 中国地质调查局地质大调查项目(1212010610706);; 国家自然科学基金项目(40771213)资助
【CateGory Index】: P532
Download(CAJ format) Download(PDF format)
CAJViewer7.0 supports all the CNKI file formats; AdobeReader only supports the PDF format.
【Citations】
Chinese Journal Full-text Database 10 Hits
1 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);Geological Characteristics and Tectonic-Sedimentary Coupling Relation of the Chishan Uplift and Anxiang Sag of Quaternary Dongting Basin[J];Acta Sedimentologica Sinica;2010-04
2 BAI Daoyuan1,2,LI Chang'an2,WANG Xianhui1,MA Tieqiu1,ZHOU Kejun1,PENG Yunyi1,LI Gang1 and CHEN Duping1(1.Hunan Institute of Geology Survey,Changsha 410011,Hunan,China;2.Faculty of Earth Sciences,China University of Geosciences,Wuhan 430074,Hubei,China);Quaternary Tectonic Characteristics and Dynamic Mechanisms of the Dongting Basin[J];Geotectonica Et Metallogenia;2010-03
3 BAI Dao-yuan1,NI Yan-jun1,LI Song-wen2,MA Tie-qiu1,WANG Xian-hui1,PENG Yun-yi1,LI Gang1(1.Hunan Institute of Geological Survey,Changsha 410011,Hunan,China;2.No.418 Geological Party,Hunan Bureau of Geology and Mineral Exploration and Development,Loudi 417100,Hunan,China);A geometrical and kinematic analysis of the Early-Mesozoic Yueyang-Chibi fold-thrust belt in southern Jiangnan orogen[J];Geology in China;2009-05
4 BAI Dao-yuan1, LI Song-wen2, ZHOU Ke-jun1, MA Tie-qiu1, WANG Xian-hui1, PENG Yun-yi1, LI Gang1 (1. Hunan Institute of Geological Survey, Changsha 410011, Hunan, China; 2. No. 418 Geological Party, Hunan Bureau of Geology and Mineral Exploration and Development, Loudi 417100, Hunan, China);Tectonic-sedimentary landform classification of 1∶250000 Changde Sheet and its implication for researches on Quaternary geology and environment of Jianghan-Dongting basin[J];Geology in China;2010-02
5 BAI Dao-yuan1,2,WU Neng-jie1,LI Chang'an2,MA Tie-qiu1,WANG Xian-hui1,PENG Yun-yi1,LI Gang1,CHEN Du-ping1(1.Hunan Institute of Geological Survey,Changsha 410011,Hunan,China;2.Faculty of Earth Sciences,China University of Geosciences,Wuhan 430074,Hubei,China);Quaternary tectonic and sedimentary characteristics and geological evolution of the Huarong uplift and its adjacent areas[J];Geology in China;2010-05
6 Zhang Shufu Xiao Jiayi (Nanjing Normal University) Yu Lizhong (Liverpool University, U.K.) Wu Yushuc (Institute of Botany, Academia Sinica, Beijing);MINERAL MAGNETIC MEASUREMENT OF LAKE SEDIMENTS AND ITS ENVIRONMENTAL IMPLICATION[J];Scientia Geographica Sinica;1991-02
7 Zhang Zhenke Wu Ruijin Wang Sumin (Lake Sediment and Environment Laboratory, Nanjing Institute of Geography and Limnology, Chinese Academy of Science, Nanjing 210008);IMPLICATION OF MAGNETIC FREQUENCY DEPENDENT SUSCEPTIBILITY ON ENVIRONMENTAL VARIATION FROM LACUSTRINE SEDIMENT IN DAIHAI LAKE[J];GEOGRAPHICAL RESEARCH;1998-03
8 BAI Dao-yuan1,2),LI Chang-an2),WANG Xian-hui1),MA Tie-qiu1),PENG Yun-yi1) 1) Hunan Institute of Geology Survey,Changsha,Hunan 410011;2) Faculty of Earth Sciences,China University of Geosciences,Wuhan,Hubei 430074;Tectonic Activities and Dynamic Mechanisms of the Quaternary Lixian sag of Dongting Basin[J];Acta Geoscientica Sinica;2010-01
9 Xiong Shangfa① Zhu Yuanjian①② Zhou Ru① Lu Haijian①② Ding Zhongli①(①Key Laboratory of Cenozoic Geology and Environment,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029;②Graduate University of Chinese Academy of Sciences,Beijing 100049);CHEMICAL WEATHERING INTENSITY AND ITS GRAIN-SIZE DEPENDENCE FOR THE LOESS-RED CLAY DEPOSIT OF THE BAISHUI SECTION,CHINESE LOESS PLATEAU[J];Quaternary Sciences;2008-05
10 FENG Lian-jun, CHU Xue-lei, ZHANG Qi-rui, ZHANG Tong-gang Institute of Geology and Geophysics , Chinese Academy of Science, Chinese Key Lab of Mineral Resources Exploration and Research , Beijing 100029, China;CIA (CHEMICAL INDEX OF ALTERATION)AND ITS APPLICATIONS IN THE NEOPROTEROZOIC CLASTIC ROCKS[J];Earth Science Frontiers;2003-04
【Co-citations】
Chinese Journal Full-text Database 10 Hits
1 WANG Qiu-xiao et al (Graduate School,China University of Geosciences (CUG),Wuhan,Hubei 430074);Environmental Magnetic Susceptibility and Granularity Analysis in the Tonglvshan Mine Area[J];Journal of Anhui Agricultural Sciences;2010-11
2 Cheng Guodong, Wang Shaoling ( Lanzhou Institute of Glaciology and Cryopedology, Academia Sinica );ON THE ZONATION OF HIGH-ALTITUDE PERMAFROST IN CHINA[J];Journal of Glaciology and Geocryology;1982-02
3 Huang Peihua ( Deparment of Earth and Space Sciences, University of Science and Technology of China );RESEARCH AND CONTENTION ON THE QUATERNARY GLACIATION PROBLEM OF EAST CHINA DURING LAST 50 YEARS[J];Journal of Glaciology and Geocryology;1983-02
4 Cui Zhijiu (Department of Geography, Beijing University) Xie Youyu (Institute of Geography, Academia Sinica);Argument on and Future of the Problems of the Pleistocene Glaciers in the Eastern Part of China[J];Journal of Glaciology and Geocryology;1984-03
5 Nie Guoxiang (Hospital for the Prevention and Cure of Schistosomiasis, Hunan Province);Discussion on the Quaternary Climate in East China from the Distribution of Oncomelania in the Middle Lower Reaches of the Changjiang River[J];Journal of Glaciology and Geocryology;1984-04
6 Peng Hanxing (Hehai University, Nanjing);Disecussion on the Formatation of the Debris Flow of the Red Bounder Clay in the Lushan[J];Journal of Glaciology and Geocryology;1990-01
7 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
8 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
9 YANG Xiao qiang 1,2 LI Hua mei 2 1 (Department of Earth Sciences, Sun Yat Sen University, Guangzhou 510275) 2 (Guangzhou Institute of Geochemistry, CAS, Guangzhou 510640);The Correlation between the Content of the Different Grain Size and Magnetic Susceptibility in Lacustrine Sediments, Nihewan Basin[J];Acta Sedimentologica Sinica;2002-04
10 LAI Hong-zhou MO Duo-wen LI Xin-po (College of Environmental Sciences, Peking University, Beijing 100871);Research on the Quaternary Laterite and Paleoclimate in the Dongting Basin[J];Acta Sedimentologica Sinica;2005-01
China Proceedings of conference Full-text Database 5 Hits
1 AO Hong~(1,2) 1 Paleomagnetism and Geochronology Laboratory(SKL-LE),Institute of Geology and Geophysics, Chinese Academy of Sciences,Beijing 100029,China 2 Graduate University of Chinese Academy of Sciences,Beijing 100049,China;Rock magnetic properties of the fluvio-lacustrine sediments from the Dachangliang section in the Nihewan Basin,northern China[A];[C];2009
2 Luo Baoxin Wang Yuzhao (Tianjin Institute of Geology and Mineral Resources) Lin Zerong (Changchun College of Geology) Dai Guozi (Bureau of Geology and Mineral Resources of Hebei Province) Hu Jilan (Bureau of Geology and Mineral Resources of Inner Mongol Autonomous Region);THE PRELIMINARY RESEARCH ON QUATERNARY PALYNOLOGY IN CHINA[A];[C];1985
3 Yang Dayuan (Nanjing University);NEW VIEWPOINT ON PLEISTOCENE GLACIATION IN THE LUSHAN MOUNTAIN[A];[C];1985
4 Liu Youmin Wang Guizeng;RESEARCH ON QUATERNARY GLACIAL GEOLOGY IN QINLING MOUNTAIN[A];[C];1987
5 Yin Chongyu~1 Gao Linzhi~1 Xing Yusheng~1 Wang Ziqiang~2 Tang Feng~1 1 Institiute of Geology,Chinese Academy of Geological Sciences,Beijing 100037; 2 China University of Geosciences,Beijing 100080;ADVANCES IN THE STUDY ON THE NANHUA SYSTEM OF THE NEOPROTEROZOIC AND ITS STRATOTYPE IN SOUTH CHINA[A];[C];2004
【Secondary Citations】
Chinese Journal Full-text Database 10 Hits
1 MAO De\|hua\+\{1, 3\},\ XIA Jun\+\{2, 3\} (1. College of Resources and Environment, Hunan Normal University, Changsha Hunan 410081, China; 2.College of Hydraulic and Electric Engineering, Wuhan University, Wuhan Hubei 430072, China; 3. Institute of Geo;Ecological and Environmental Problems and Their Causing Mechanisms in Dongting Lake Wetland[J];Journal of Glaciolgy and Geocryology;2002-04
2 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
3 GONG Shengsheng (Department of Geography, Central China Normal University, Wuhan 430079,China);HISTORICAL VARIATION AND SUSTAINABLE UTILIZATION OF THE JIANGHAN-DONGTING PLAIN'S WETLANDS[J];Resources and Environment in the Yangtze Basin;2002-06
4 YANG Gui-fang1, PENG Hong-xia2, CHEN Zhong-yuan1 LI Chang-an2, HUANG Jun-hua2, HU Chao-yong2 (1.Department of Geography, East China Normal University, Shanghai 200062, China; 2.Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China );PALEOCLIMATIC IMPLICATIONS OF LANZHOU AND JIANGHAN PLAIN: A CLIMATE PROXY STUDY OF ORGANIC CARBON ISOTOPE[J];Resources and Environment in the Yangtze Basin;2005-04
5 DENG Hong-bing~1,2,CAI Shu-ming~3,DU Yun~3,XUE Huai-ping~3,WEI Xian-hu~3(1.Faculty of Humanity and Economy,China University of Geosciences,Wuhan 430074,China;2.School of Business,Wuhan University,Wuhan 430072,China;3.Institute of Geophysics,The Chinese Academy of Sciences,Wuhan 430077,China);QUANTITATIVE ANALYSIS ON THE EVOLUTION OF JIANGHAN LAKES REGION OVER THE LAST 50 YEARS[J];Resources and Environment in the Yangtze Basin;2006-02
6 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
7 ZHAO Hong-ge LIU Chi-yang (Department of Geology of Northwest University,Xi’an 710069 );Approaches and Prospects of Provenance Analysis[J];Acta Sedimentologica Sinica;2003-03
8 WANG Yong hong 1 SHEN Huan ting 2 ZHANG Wei guo 2 1(Ocean University of China, College of Marine Geosciences, Qingdao,Shandong 266003) 2(East China Normal University, State Key Laboratory of Estuarine and Coastal Research, Shanghai 200062);A Preliminary Comparison of Magnetic Properties of Sediments from the Changjiang and the Huanghe Estuaries[J];Acta Sedimentologica Sinica;2004-04
9 LAI Hong-zhou MO Duo-wen LI Xin-po (College of Environmental Sciences, Peking University, Beijing 100871);Research on the Quaternary Laterite and Paleoclimate in the Dongting Basin[J];Acta Sedimentologica Sinica;2005-01
10 WANG Zhong-bo~(1,2) YANG Shou-ye~(2) LI Ping~(2) LI Cong-xian~(2) CAI Jin-gong~(2)(1.Qingdao Institute of Marine Geology,Qingdao,Shandong 266071;2.State Key Laboratory for Marine Geology,Tongji University,Shanghai 200092);Detrital Mineral Compositions of the Changjiang River Sediments and Their Tracing Implications[J];Acta Sedimentologica Sinica;2006-04
©2006 Tsinghua Tongfang Knowledge Network Technology Co., Ltd.(Beijing)(TTKN) All rights reserved