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《GEOSCIENCE》 1999-01
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PERMIAN SEQUENCE SUCCESSIONS OF SLOPE FACIES IN SOUTHERN GUIZHOU AND THEIR CHRONOSTRATIGRAPHIC CORRELATION

Shi Xiaoying Mei Shilong Sun Yan Li Bin Sun Keqin(China University of Geosciences, Beijing, 100083)  
The Permian in slope facies area of southern Guizhou consists of sixteen 3rd order sequences, which can be grouped into four sequence sets.Most of the sequences are delineated by continuity surfaces, and are precisely controlled by conodont and fusulinid zones.Four important sea level falls have been recognized in the area, which occurred respectively at the positions corresponding to the bottom of conodont Sw whitei zone, lower part of Sw aff hanzhongensis zone, middle part of J Xuanhanensis zone and the base of Cl yini zone.Among the recognized transgressions, three are regarded as the most significant ones.They occur respectively at the bottom of conodont N exculptus zone, base of J nankingensis zone and the lower part of J pos tbitteri zone, and are all accompanied with faunal turnovers.The key surfaces in depositional sequences have the potentials of fine tuning the boundaries of stages and biozones.
【Fund】: 国土资源部“九五”重大基础研究项目 国家“九五”攀登专项
【CateGory Index】: P534.46
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