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《Acta Geologica Sinica》 2008-05
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Clay Minerals of the Middle-Late Mesozoic Mudrocks from North and Northeast China:Implications to Paleoclimate and Paleohighland

LI Xianghui1), XU Baoliang2), CHEN Yunhua2), CAO Ke2), YANG Hainan3) 1) Department of Earth Sciences, Nanjing University, Nanjing, 210093; 2) Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu, 610059; 3) The First Oil Factory, Changqing Oilfield Company, SINOPEC, Jingbian,Shanxi, 718500  
Four clay minerals of the middle and late Meesozoic mudrock samples from North and Northeast China were analyzed by TEM and Illite Crystallinity (IC) in the study. The paper also explained the reliability of experimental data when employed to analyze paleoclimate. Spatial and temporal change of contents of clay minerals, features and evolution of paleoclimate, as well as the relation between the change and paleohighland, were also discussed in the research. The result shows that illite is the most common clay mineral in the study area during the Middle and Late Mesozoic. The contents in each study area is no less than 20% (averaging to 46.6%). The content of smectite ranks the second with an average of 57.8% in Henan and Shandong provinces. Both kaolinite and chlorite are less common in most the study area, but relatively abundant in Shanxi province, indicating that the studied area was dry and cold during middle and later Mesozoic time, except that climate in Shanxi changed between dry cold and humid. This, to some extent, demonstrate ancient highland was there, i.e., the "East China Paleo Plateau". However, there are some differences in both time duration and space distribution between the the "highland" and "plateau" although it is temporally cited as "plateau". Herein the "Eastern China paleo Plateau" is defined as a highland developed from Middle Jurassic through Cretaceous (even to the end of the Paleogene) in North and southeastern and Northeast China. It is confined in Shanxi, Henan and Shandong provinces in early stage (Middle Jurassic) and spreaded to eastern Liaoning province in middle late stage (Late Jurassic and Cretaceous). It is proposed that the plateau had not influenced all the Northeast China during the time, and could alter the climate in northern Hebei and western Liaoning in Late Jurassic and Late Cretaceous. In addition, it is also suggested that the matter in the plateau could be transported into the paleo Pacific ocean by two outlets at the end of the Tanlu strike slip fault in Middle Jurassic and Early Cretaceous, and most of the plateau could be eroded and transported into sedimentary basins around the highland.
【Fund】: 国家重大基础研究发展规划项目(973)课题“中国白垩纪重要时期的古气候重建”(编号2006CB701401)资助成果
【CateGory Index】: P532
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Chinese Journal Full-text Database 10 Hits
1 ZHANG Yun FANG Xiaosi(College of Life Science, Peking University,Beijing,100871);A Late Cretaceous Dinosaur Egg with Preserved Genetic Information from XiXia Basin ,Henan,China:Structure,Mineral-Chemical and TaphonomicaI Analyses[J];ACTA SCICENTIARUM NATURALUM UNIVERSITIS PEKINESIS;1995-02
2 Zhang Chuanbo Zhao Dongpu Zhang Xiuying Ding Qiuhong(Changchun University of Earth Science, Changchun}Yang Chunzhi Shen De'an(First Geology Survey, Geolodv and Mineral Resources Bareau of Jilin Province);THE COAL-BEARING HORIZON OF THE LATE MESOZOIC IN THE EASTERN EDGE OF THE SONGLIAO BASIN, JILIN PROVINCE[J];;1991-03
3 You Zonghua (Third Institute of Oceanography, National Bureau of Oceanography, Xiamen);PRELIMINARY STUDY ON THE CLAY MINERALS OF SEDIMENTS IN THE MIDDLE OF THE PACIFIC OCEAN[J];Acta Sedimentologica Sinica;1985-03
4 Liu Guanghua (Beijing Graduate School, Wuhan College of Geology);STUDY OF THE RELATIONSHIP BETWEEN CHARACTERISTICS OF CLAY MINERALS AND DEPOSITIONAL ENVIRONMENTS[J];Acta Sedimentologica Sinica;1987-01
5 LIU Hao WANG Ying-min WANG Yuan (The Petroleum University of Beijing,Basin and Oil Research Center,Beijing 102249);Analyses of the Significances of Jurassic Coal Layers in Sequence Stratigraphy in Junggar Basin[J];Acta Sedimentologica Sinica;2002-02
6 Deng Yangxin(Lanzhou Institute of Glaciology and Geocryology, Chinese Academy of Sciences, Lanzhou 730000);Process of Accumulation and Characteristics of Glacial Debris Flow Deposits Trangformed by Moraine[J];ACTA SEDIMENTOLOGICA SINICA;1995-04
7 Qiu Song-yu;Anda Formation in the northern Songliao basin and its spore-pollen assemblage[J];Journal of Stratigraphy;1992-01
8 Zhu Fengguan (The Second Institute of Oceanography, National Bureau of Oceanography);Clay Minerals of the East China Sea Shelf Area in the Recent Epoch Stratum[J];Donghai Marine Science;1985-04
9 LIAO Rui-jun 1 ,ZHONG Cun-di 2 and XIAO Xiao-lin 2(1.Western Jiangxi Geological Survey Party,Jiangxi Bureau of Geology and Mineral Exploration,Xiang tang,Nanchang3302012.Jiangxi Institute of Geological Survey,Xiangtang,Nanchang330201,Jiang;Lithostratigraphic sequence boundaries in regional geological mapping of terrestrial red basins in Jiangxi[J];Chinese Geology;2001-10
10 Ching Hua Lo① Chen Pei ji ② Tung Yu Tsou① Shen su Sun③ Chi Yu Lee①(①Department of Geology, National Taiwan University, Taibei 106 17)(②Nanjing Institute of Geology and Paleontology, Chinese Academy of Sciences, Nanjing 210008)(③16 Giff;Age of Sinosauropteryx and Confuciusornis——~(40)Ar/~(39)Ar laser single grain and K Ar datingof the Yixian Formation, NE China[J];GEOCHIMICA;1999-04
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