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《Journal of Stratigraphy》 2003-03
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REVISION AND CHARACTERS OF THE POYANGHU FORMATION (QUATERNARY)

MA Zhen xing 1) , JIANG Yu zhen 2) , WEI Yuan 1) , LI Jun hui 1) , and LI Chang an 3) ( 1)Geological Survey of Jiangxi Province, Nanchang, 330201; 2) Geological Survey Brigade of West Jiangxi, Nanchang, 330201; 3) Chine University of Geosciences, Wuhan, 430074)  
The Poyanghu Formation was proposeod in 1997 by the Geological Survey and Study Brigade of Jiangxi Province, originally donoting the latest lacustrine deposits of the Holocene in the Poyanghu area. This formation has been so for less studied that its lithostratigraphical divisions are not very reasonable and the sedimentary fine range is vague. Based on the study of the columnar section, Zk01 borehole in the Poyanghu area, a revision of the lithostratigraphical units of the Poyanghu Formation is made in this paper. It is regarded that the Poyanghu Formation is composed dominantly of blue grey muddy clay, yellow brown clay and silty clay intercalated with a small number of silty of sandy sediments of lacustrine—estuarine delta facies, with a basic boundary being about 6 210±125a B.P. The open lake began to be deposited at an age of 3 246±180a B.P. and became younger southwards, with a prominent diachronism. It belongs to the Holocene (Quaternary) in chronostratigraphy.
【Fund】: 中国地质调查局长江中游江西段主要水患区环境地质调查评价项目(编号:1999160 0 0 114 )的部分成果
【CateGory Index】: P534.63
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