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LOWER PLEISTOCENE SERIES IN JIANGHAN PLAIN

Chen Huahui Ma Zulu (Wuhan College of Geology, Wuhan 430074)  
Based on the systematic researches of Quaternary geology in Jianghan plain, the authors have reestablished the Quaternary stratigraphic time-scale of this area, and first established and discussed the Lower Pleistocene-Luyanchong Formation and Yangluo Formation in detail. The two Formations scattered over this area and constituted the V-stepped or IV-stepped terraces of the Yangtze River. Based on the lithological characteristics, morphological display, genetic sequence, diagenetic degree, paleontogic facies and structural relations, the two Formations may be distinguished from the Neogene system-Shihuiqiao Formation, and also do from the widely spread gravel beds. The above-mentioned might help to recover the Early Pleistocene's palaecgeographic character, especially the evolutional history of the Yangtze Rivetr and solve the problem of the lower boundary of the Quaternary.
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