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《Journal of Hefei University of Technology(Natural Science)》 2005-09
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Study on alluvial sediments of Early Cretaceous Zhougongshan Formation in the northern margin of the Dabie orogenic belt

LI Shuang-ying~1,YUE Shu-cang~1,WANG Dao-xuan~1,LIU Yin~1,LI Ren-wei~2(1.School of Resources and Environment,Hefei University of Technology,Hefei 230009,China;2.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China)  
The Early Cretaceous Zhougongshan Formation(ZgsF.),which developed in the Feixi-Lu'an region,Anhui Province and is above 800 meters thick,comprises mainly fine-to coarse-grained sandstone,mudstone and siltstone,and a little conglomerate.According to Miall's facies classification,it consists of twelve kinds of facies,and the main facies are Gci,Gcm,Ss,St,Sp,Sh,Sm,Fsm and Fm. Six architectural elements such as channel lag deposit,meander sandy bars,levees,crevasse splay and floodplain fine are distinguished,among which crevasse splay and floodplain fine are most abundant.According to stream features of 16 kinds proposed by Miall,it is believed that the lower member of ZgsF.belongs to sediment of fine-grained meandering streams and the upper member corresponds to that of sandy meandering streams.The channel sinuosity(P) is 2.09 ~ 3.55.The channel is 31.4 ~ 81.1 meters wide.The channel meander wavelength is 385.63 ~1 025.66 meters.The change of sedimentary environment of ZgsF.might record the difference of uplift speed of the provenance,the Dabie orogenic belt.
【Fund】: 国家重点基础研究发展规划资助项目(G1999075507)
【CateGory Index】: P534.53;
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