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《GEOSCIENCE》 1999-01
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SEQUENCE STRATIGRAPHY OF PERMIAN LOPINGIAN STRATA IN CENTRAL GUANGXI

Mei Shilong 1) Zhu Zili 2) Shi Xiaoying 1) Sun Keqin 1) Li Bin 1) ( 1)China University of Geosciences, Beijing,100083;2)Nanjing Institute of Geology and Paleontology, Nanjing,210008 )  
The uppermost Yangsingian and Lopingian strata in central Guangxi is subdivided into one second order sequence, namely the Leping Sequence, and its six component third order sequences, and the corresponding sea level change curves are established, based on a comparative study on a carbonate platform section, namely the Matan Section at Heshan, a slope section, namely the Tieqiao Section at Laibin and a basinal section, namely the Penglaitan Section to the east of Laibin. The third order sequences are named in ascending order as Lp1, Lp2, Lp3, Lp4, Lp5 and Lp6. Precise correlation of these sequences among these three sections is realized, with aid of renewed biostratigraphic data. As a result,the resolution of previous correlation is raised by at least two times. It is suggested to define the Wuchiapingian Changhsingian boundary by the first appearance of a conodont species, i.e., Clarkina subcarinata. This horizon is found to be in accordance with the first flooding surface of the third order sequence Lp6. Gallowayinella meitienensis and Palaeofusulina minima , which have long been regarded as typify of the lower Changhsingian, are found ranging into the underlying Wuchiapingian.
【Fund】: 国家“九五”攀登计划 国家自然科学基金
【CateGory Index】: P534.46
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