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《JOURNAL OF STRATIGRAPHY》 1997-03
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Stratigraphic research on the lower member of the Devonian Wuzhishan Formation of Nayi,Guangxi

Liu Shengcheng (Research Center for Basin and Reservoir,University of Petroleum,Beijing, 102200)  
Based on the Late Devonian standard zonation of Ziegler et Sandberg (1990),three conodont zones are recognized in the lower member of the Devonian Wuzhishan Formation,in descending order as mixed Upper crepida Zone,mixed Middle crepida-triangularis Zone,Lower triangularis Zone.Reworked fossils are also recognized in this member,which consists of calcareous parabreccia interbedded with nodular limestones.Therefore,the lower member should be carbonate turbidite deposits,which occurred in triangularis- Upper crepida Zone, Famennian.Moreover,the lower member is considered to be deposited near the slope in an episcalic basin,it is believed that at least two kinds of turbidites exist in the member.In addition,many microspheres are recognized in this member.
【CateGory Index】: P534.53(6)
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