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《Geology and Mineral Resources of South China》 2010-04
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Statistics of Gravel Particle Size and Shape Features of Middle Pleistocene Dongtinghu Formation in Dongting Basin,and Its Tectonic and Environmental Significances

CHEN Jian-cheng1,BAI Dao-yuan2,LI Chang-an3,ZHOU Ke-jun2,HUANG Wen-yi2,CHEN Du-ping2(1.No.413 Brigade of Hunan Bureau of Geology and Mineral Exploration and development,Hunan Changde 415000,China;2.Hunan Institute of Geology Survey,Changsha 410011,China;3.Faculty of Earth Sciences,China University of Geosciences,Wuhan 430074,China)  
The statistics and analysis of gravel particle size and shape features of Middle Pleistocene Dongtinghu Formation from Lianghucun ZKC1 borehole in southeastern Anxiang sag of Dongting basin were taken in this paper.The variations of gravel particle size show two big-to-small cycles whose early cycle corresponded with the lower member of Dongtinghu Formation and late cycle corresponded with upper part of the middle member of Dongtinghu Formation.The two particle size cycle indicate two slow-to-rapid episodic subsidence of Anxiang sag during early-middle Middle Pleistocene.Superposed on the two large cycles there existed a lot of small scale variations of gravel particle size which were mainly related to aridity-humidity changes.The roundness of gravels from top of middle member of Dongtinghu Formation is evidently low,which indicated strengthen of tectonic movement such as subsidence of the basin and rise of around uplifts.
【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(批准号:40771213)资助
【CateGory Index】: P534.631
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