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《Tropical Geography》 2008-02
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Development Periods and Mechanism of the Red Weathering Base of Alluvial Terraces: An Instance Study of the 6 Class Alluvial Terraces in Pingshi Basin of North Guangdong

LIU Kun,GAO Quan-zhou,JIAO Shu-lin,WANG Zhen-gang,SHE Jian-wei,DING Jian(School of Geography and Planning,Sun Yat-sen University,Guangzhou 510275,China)  
Total six classes of rock-based alluvial terraces are discovered in Pingshi Basin of the Wujiang River,Guangdong,which are the most classes of terraces in the province.The rock-bases of the terraces affected by the chemical weathering have developed into deep-thick red weathering bases,which are special weathering crust covered by alluvium.The alluvium,as the product of floodwater,reflects the intensity of the fluviation and the summer monsoon.The development of weathering base was influenced by the tectonic rise during the mid-Pleistocene and summer monsoon together.The TL data of the alluvial terracesi,ncluding(819±57)kaBP,(694±55)kaBP,(426±29)kaBP,(163±11)kaBP,show that the development time of the weathering rock-bases in Pingshi Basin accorded with the temporal-spatial characteristics of the Red Earth Period in South China,but its formation mechanism was different from that of the weathering crusts of corresponding terraces in the area,and it was mainly affected by the regional tectonic rise.The weathering rock-bases in Pingshi Basin developed one more class of terrace as compared with other places in South China during Q12 and Q22,and T1 in Pingshi Basin was formed during late mid-Pleistocene,earlier than that in other places of South China.When the red weathering crusts were developing in South China,the debris flow activation in western China also came forth many periods.As a whole,not only the development periods of debris flow were later than those of the red earth,but also its frequencies were less during the same period,indicating that the effect of summer monsoon on red earth development was more intense than that on the debris flow,when summer monsoon was intensified,and the hydro-cycle was quickened and chemical weathering reinforced.The climatic environment and tectonic movement offered the possibility to develop the double-layer planation surface in Pingshi Basin.The covered weathering rock-base may be a double-layer planation surface developed in sandstone areaI.f that is truei,t means that double-layer planation surface can develop in any kind of rock under suitable environment.The mid-Pleistocene is an important period for the weathering rock-bases development,when the tectonic movement was active and the summer monsoon was strong.
【Fund】: 国家自然科学基金(40671027);; 高等学校博士学科点专项科研基金(20040558025);; 广东省自然科学基金(7003669)资助
【CateGory Index】: P512.31
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【Citations】
Chinese Journal Full-text Database 10 Hits
1 Yang Dayuan Wu Shengguang (Dept. of Geo. and Ocean Science, Nanjing University, Nanjing 210093)Wang Yunfei (Nanjing Institute of Geography and Limnology, Academia. Sinica, Nanjing 210008);ON RIVER TERRACES OF THE UPPER REACHES OF THE HUANGHE RIVER AND CHANGE OF THE RIVER SYSTEM[J];Scientia Geographica Sinica;1996-02
2 HUANG Zhen-Guo~1,ZHANG Wei-Qiang~2 (1.Guangzhou Institute of Geography,Guangzhou 510070,China, 2.Guangdong Business College,Guangzhou 510320);Geomorphological Effects of Plate Movement During Quaternary in China′s Tropics[J];Scientia Geographica Sinica;2004-03
3 HUANG Zhen guo, ZHANG Wei qiang (Guangzhou Institute of Geography, Guangzhou 510070);Coupling Relationship between the Red Earth Evolution, Climate Change and Tectonic Movement in China[J];ACTA GEOGRAPHICA SINICA;2000-02
4 LI Dewen 1) CUI Zhijiu 2) LIU Gengnian 2) ( 1)Nanjing University, Nanjing, Jiangsu, 210093; 2)Peking University, Beijing, 100871);Present Situation and Prospects of Researches on Weathering Crust[J];Acta Geosicientia Sinica;2002-03
5 Yuan Fuli;MULTILAYERED LANDFORMS IN NANLING MOUNTAIN RANGE AND THEIR RELATED THEORETICAL PROBLEMS[J];Quaternary Sciences;1993-04
6 Zhu Zhaoyu, Xu Yifang, Wen Qizhong, Pu Zhiping, Zhou Houyun Wen Gaoguo, Dai Tongmo, Liang Junping, Liang Chisheng, Luo Shuwen (Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640; Bureau of Geology and Mineral Resources of G;THE STRATIGRAPHY AND CHRONOLOGY OF MULTICYCLE QUATERNARY VOLCANIC ROCK-RED SOIL SEQUENCE IN LEIZHOU PENINSULA, SOUTH CHINA[J];Quaternary Sciences;2001-03
7 Li Yonghua ① Zhang Xiaoyong ① Cui Zhijiu ② Gao Quanzhou ③ (①Urban and Environment Sciences Institute of Liaoning Normal University, Dalian 116029; ② Urban and Environment Sciences Department of Peking University, Beijing 100871; ③ Earth and Environment Sciences Department of Zhongshan University, Guangzhou 510275 );PERIODIC COUPLING OF DEBRIS FLOW ACTIVE PERIODS AND CLIMATE PERIODS DURING QUATERNARY[J];Quaternary Sciences;2002-04
8 Pan Baotian ① Gao Hongshan ① Li Bingyuan ② Li Jijun ① (① Key Laboratory of Western China’s Environmental Systems, Ministry of Education & Department of Geography, Lanzhou University, Lanzhou 730000; ②Institute of Geographical Science and Natural Resource, Chinese Academy of Sciences, Beijing 100101);STEP-LIKE LANDFORMS AND UPLIFT OF THE QINGHAI-XIZANG PLATEAU[J];Quaternary Sciences;2004-01
9 SUN Cheng xing,WANG Shi jie,LIU Xiu ming,JI Hong bing (State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002,China);Review on the Dating of the Weathering Profiles[J];BULLETIN OF MINERALOGY PETROLOGY AND GEOCHEMISTRY;2000-01
10 Huang Zhenguo; Zhang Weiqiang; Chen Junhong(Guangzhou Institute of Geography, Guangzhou 510070);THE RED EARTH PERIODS IN CHINA[J];TROPICAL GEOGRAPHY;1998-01
【Co-citations】
Chinese Journal Full-text Database 10 Hits
1 ZHANG Li-yun et al(Institute of Geographical Sciences,The Hebei Academy of Sciences,Shijiazhuang,Hebei 050011);The Scientific Significance of Dianziliang Oligocene Planation Surface in Hebei Province[J];Journal of Anhui Agricultural Sciences;2011-11
2 GAO Hong-shan~(1),PAN Bao-tian~(1),WU Guang-jian~(2,3),LI Ji-jun~(1), GUAN Qing-yu~(1),WANG Jun-ping~(1),YE Yu-guang~(4) n, Lanzhou University, Lanzhou Gansu 730000, China; 2.Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beiof Ice Core and Cold Regions Environment, CAREERI, CAS, Lanzhou Gansu 730000, China; 4.Institute of Marine Geology, Ministry of Land and Resources, Qingdao Shandong 266071, China);Erosion Surfaces in the East Qilian Mountains and Uplift of the Tibetan Plateau[J];Journal of Glaciology and Geocryology;2004-05
3 ZHOU Shang-zhe,LIU Ji-peng,XI Zeng-fu,ZHOU Ling-yun(School of Geographical Science,South China Normal University,Guangzhou Guangdong 510631,China);The Residual Top Planation Surfaces in the Nanling Mountains and Their Adjacent Regions[J];Journal of Glaciology and Geocryology;2008-06
4 WANG Dechao,ZHANG Jinjiang,YANG Xiongying,QI GuoweiThe Key Laboratory of Orogenic Belts and Crustal Evolution,Ministry of Education,School of Earth and Space Sciences,Peking University,Beijing 100871;;Tectonic and Environmental Evolution of Gyirong Basin,and its Relationship to the Uplift of Tibetan Plateau[J];Acta Scientiarum Naturalium Universitatis Pekinensis;2009-01
5 LIU Kui1,ZHUANG Zhen-ye2,LIU Dong-yan2,YE Yin-can11.The Second Institute of Oceanography,SOA,Hangzhou 310012,China2.College of Marine Geosciences,Ocean University of China,Qingdao,Shandong 266100,China;Hydrology Environment Characteristics of Buried Ancient Channels near Zhoushan Islands and Yangtze River Estuary[J];Journal of Jilin University(Earth Science Edition);2010-01
6 REN Shou-mai1,MENG Jing-yao2,LIN Yuan-xian3, JIANG Wen-li1,QIAO De-wu1,HE Ming4,ZUO Tian-wen5 1.Strategic Research Center of Oil & Gas Resources,Ministry of Land & Resources,Beijing 100034,China 2.College of Earth Sciences,Jilin University,Changchun 130061,China 3.Tianjin Institute of Geology and Mineral Resources,Tianjin 300170,China 4.Department of Nuclear Physics,China Institute of Atomic Energy,Beijing 102413,China 5.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;Grain Size Analysis and ~(36)Cl Dating of Early Pleistocene Sediments of Dunhuang Basin,Tectonic Uplift Implication[J];Journal of Jilin University(Earth Science Edition);2011-05
7 WANG Yun-sheng,HUANG Run-qiu,DUAN Hai-peng,WEI MengGeological Hazards and Environment Protection National Speciality Lab.,Chengdu University of Technology,Chengdu 610059,China;An intensive erosion event in the last glaciation in the west of China[J];Journal of Chengdu University of Technology(Science & Technology Edition);2006-01
8 ZHENG Yue-rong1,2,LI Yong2 1.College of Earth Sciences,Chengdu University of Technology,Chengdu 610059,China;2.Faculty of Geography and Resources Sciences,Sichuan Normal University,Chengdu,610066,China;Study on the denudation rate,incision rate,uplifting rate of the Three Gorges of the Yangtze River in short-period[J];Journal of Chengdu University of Technology(Science & Technology Edition);2010-05
9 HE Qi-xiang (Qingdao Institute of Marine Geology, Qingdao Shandong 266071);Sedimentary Earth Sciences:Yesterday, Today and Tomorrow[J];Acta Sedimentologica Sinica;2003-01
10 BAI Chun-guang WANG Jian (College of Geographical Sciences, Nanjing Normal University, Nanjing 210097);A New Grain-size Index: Grain-size Fractal Dimension of Sediment and Its Environmental Significance[J];Acta Sedimentologica Sinica;2003-02
China Proceedings of conference Full-text Database 5 Hits
1 Yuan Baoyin~①Guo Zhengtang~①Hao Qingzhen~①Peng Shuzhen~(①②) Qiao Yansong~③Wu Haibin~④Xiao Guoqiao~(④⑤) Ge Junyi~(④⑤) Sun Bin~(①⑤) Zhou Xin~(④⑤) Yin Qiuzhen~(①⑤) Liang Meiyan~(①⑤)Qin Li~(①⑤) Liu Lian~(①⑤) Yao Zhengquan~(④⑤) Liu Tungsheng~①(①Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029;②Taishan College,Tai'an 271021;③Institute of Geomechanics,Chinese Academy of Geological Sciences,Beijing 100081;④Institute of Earth Environment,Chinese Academy of Sciences,Xi'an 710075;⑤Graduate University of Chinese Academy of Sciences,Beijing 100049);CENOZOIC EVOLUTION OF GEOMORPHIC AND SEDIMENTARY ENVIRONMENTS IN THE TIANSHUI-QIN'AN REGIONS[A];[C];2008
2 Yin Qiuzhen~(①③) Xiao Guoqiao~(②③) Guo Zhengtang~①Ge Junyi~(②③)Hao Qingzhen~①Yuan Baoyin~①(①Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029;②State Key Laboratory of Loess andQuaternary Geology,Institute of Earth Environment,Chinese Academy of Sciences,Xi'an 710075;③Graduate University ofChinese Academy of Sciences,Beijing 100049);SYN-AND POST-DEPOSITIONAL MODIFICATION OF LOESS DEPOSITS AND THEIR PALEOENVIRONMENTAL SIGNIFICANCE[A];[C];2008
3 XU YingXia,QIN KeZhang,DING KunShou,LI JinXiang,MIAO Yu,FANG TongHui,XU XingWang,LI DaMing and LUO XiuQuan 1.Key Lab.of Mineral Resources,Institute of Geology and Geophysics,CAS,Beijing 100029,China 2.Department of Geology,Hebei Polytechnic University,Tangshan 063009,China 3.Beijing Institute of Geology for Mineral Resources,Beijing 100012,China 4.Institute of Geology,China Earthquake Administration,Beijing 100029,China 5.Petroleum Geology Research and laboratory Center,RIPED,Beijing 100083,China;Geochronology evidence of Mesozoic metallogenesis and Cenozoic oxidation at Hongshan HS-epithermal Cu-Au deposit,Kalatage region,eastern Tianshan,and its tectonic and paleoclimatic significances[A];[C];2009
4 Feng Shaohua~(①②) Tang Zihua~①Wang Xu~①Yang Shiling~①(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);ORIGIN AND AGE OF'RED CLAY'SEDIMENT AT JUNGAR BANNER,INNER MONGOLIA,AND ITS PALAEOCLIMATIC IMPLICATIONS[A];[C];2011
5 GUO Jinjing HAN Wenfeng LI Xuefeng (Department of Civil engineering,Tianjin Institute of Urban construction,Tianjin 300389);THE CHARACTERISTICS OF THE FAULT SYSTEM AND ITS CONTROLLING FOR THE GEOLOGICAL HAZARDS IN THE WESTERN QINLING[A];[C];2008
【Secondary Citations】
Chinese Journal Full-text Database 10 Hits
1 Guo Dongxin, Li Zuofu (Lanzhou Institute of Glaciology and Cryopedology, Academia Sinica);PRELIMINARY APPROACH TO THE HISTORY AND AGE OF PERMAFROST IN NORTHEAST CHINA[J];Journal of Glaciology and Geocryology;1981-04
2 Ma Qiuhua He Yuanqing ( Lanzhou Institute of Glaciology and Geocryology, Chinese Academy of Sciences );Moraine Features and Ice Ages of the Quaternary in the Taibai Mountain[J];Journal of Glaciology and Geocryology;1988-01
3 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
4 Cao Jiaxin Wu Ruijin (Department of Geography);The Origin and Age of The Red Loam in S. E. Shansi Province[J];Acta Scicentiarum Naturalum Universitis Pekinesis;1984-05
5 Yue Leping (Department of Geology, Northwest University, Xi'an 710069);Depositional Ralation between the Loess, Red Clay and Sedimtation of the Lakebasin in the Loess Plateau[J];ACTA SEDIMENTOLOGICA SINICA;1996-04
6 Cao Zhenglin 2 Zhao Xikui 2 Wang Yingmin 1 and Jiang Feng 21(Chengdu Institute of Technology,610059)2 (Lanzhou Institute of Geology,Chinese Academy of Sciences, 730000);Modelling Reseach on The Rock-Fluid Reaction Dynamics of The Fossil Crust of Weathering in The North of Ordos Basin[J];Acta Sedimentologica Sinica;1997-04
7 Liu Yun Wang Zong-zhe;The petrographic characters and environmental analysis of the Cretaceous-Tertia-ry Boundary strata at the Nanxiong Basin Guangdong[J];Journal of Stratigraphy;1986-03
8 Li Shoujun Xie Chuanli (Department of Petroleum Resources Science, University of Petroleum, Dongying,257062);A discussion on the age of the Laiyang Formation in Laiyang Basin,Shandong[J];JOURNAL OF STRATIGRAPHY;1997-03
9 XIE Yuan-yun 1,2 ,ZHANG Xu-qiang 2 ,HE Kui 2 ,LI Chang-'an 1 ;(1.Institute of Eorth Science,China University of Geoscicnces Wuhan4 30074,Hubei,China2.Geography department ,Harbin Normal University,Har bin150080,Heilongjiang,China);Grain-size distribution and material source analysis of loess on the nort heastern margin of the Qinghai-Tibet Plateau[J];Chinese Geology;2002-03
10 Yang Guohua and Ma Qing(No. 1 Crustal Deformation Monitoring Gentre,S. S. B);PRESENT VERTICAL CRUSTAL MOVEMENT AND ITS GRADIENT IN THE MAINLAND OF CHINA UNDER THE FLUX-ISOSTATIC DATUM AND SOME RELATIONS BETWEEN THEM AND TECTONIC ACTIVITY[J];Crustal Deformation and Earthquake;1992-04
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